造山型金矿研究进展:兼论中国造山型金成矿作用
|
摘要
造山型金矿指与大洋板块俯冲和陆块拼贴有关、产在汇聚板块边界变质地体内部或者边缘受韧-脆性断裂构造控制的,成矿流体以低盐度H_2O-CO_2-CH_4为主要特征的,成矿深度(2～20 km)和温度(200～650℃)及其相应的蚀变矿化组合有较大变化的系列金矿床.造山型金矿形成与超大陆聚合时限具有一致性.由于围岩类型和控矿构造多样性、地球化学特征具有多解性、金属源区和演化的不确定性以及成矿就位和物质起源的空间差距,造山型金矿成因模式有以下两个主要观点.第一种为大陆地壳变质流体成因模式,认为造山型金矿形成于造山作用同变质阶段,并随岩石圈演化矿床的物质来源发生变化;富金流体的释放由上地壳岩石绿片岩相到角闪岩相的进变质作用导致,该过程中的黄铁矿向磁黄铁矿转变释放了大量的金,这种模式被广泛运用于赋存在绿片岩相中的显生宙造山型金矿.然而越来越多的实例证实造山型金矿主要形成于峰期变质的退变质阶段或者与区域变质没有任何关系,变质流体成因模式受到了强烈质疑;与大陆地壳变质模式相对立的是幔源流体模式,其认为流体起源于俯冲洋壳脱水或富集地幔再活化,不同时代和地区的成矿流体具有一致性;尽管该模式不符合传统的平衡条件下的相变原理,但是基于幔源流体的存在及其浅部运移的大量观测,初步认为成矿流体是在超临界和非平衡条件下完成了金属的幔→壳迁移.中国造山型金矿分布于江南造山带志留纪、天山-阿尔泰二叠纪、华北克拉通北缘三叠-侏罗纪、特提斯造山带二叠-侏罗纪、华南板块晚三叠世-侏罗纪、华北克拉通东南缘白垩纪、青藏高原及周缘古近纪等七大成矿带,主要受到了显生宙不同时代造山作用的控制,成矿时代晚于变质峰期,重要成矿带大型矿集区(胶东、哀牢山、扬子西缘)的实例解剖均支持幔源流体成因模式.
The orogenic gold deposits show features as follows: relation to oceanic plate subduction and terrane accretion, hosted by metamorphic massif along convergent plate boundaries, controlled by ductile to brittle shear zones, low salinity and H_2 O-CO_2-CH_4 dominating ore fluid, wide formation depths varying from about 2 to 20 km and formation temperatures ranging within 200-650 ℃, temperature-dependent alteration and ore mineral assemblages. Orogenic gold deposits formed coevally to the time of cycled convergences of supercontinents. Due to the diversity of wall rock types and ore-controlling structures, ambiguity of ore geochemistry, uncertainty of fluid and metal sources and their evolutions, and disparity between source regions and ore deposition locations, two distinct origin models were proposed for orogenic gold deposits. The first is metamorphic fluid model, in which the deposits formed in prograde metamorphism of orogeny with different source from evolving regional upper crust. The auriferous fluid is considered to release from greenschist-to amphibolite-facies prograde metamorphism of upper crustal rocks,during which gold and other metals are liberated from transformation of pyrite to pyrrhotite. This model was universally applied to Phanerozoic orogenic gold deposit shosted by greenschist-facies terranes. However, it was recognized that most orogenic gold deposits formed in retrogression stage subsequent to peak metamorphism or without any spatial-temporal link to regional metamorphism, which challenged the metamorphic fluid model. Thus the mantle fluid model, which indicates that ore fluids for orogenic gold deposits are derived from devolatilization of subducted oceanic plate or fertile mantle, was proposed. Although the mantle fluid model is not compatible with the petrological diagram in phase equilibrium condition, the extensive proofs for the existence of mantle fluids and their appearance near surface support that mantle fluids are capable to transport to upper crustal levels under supercritical conditions and phase unequilibrium. The Chinese orogenic gold deposits are divided into seven gold belts: Silurian belt along Jiangnan orogen, Permian belt in Tianshan and Altay orogen, Triassic to Jurassic one along northern margin of North China craton(Solonker orogen), Triassic to Jurassic one within Paleo-Tethyan orogens, Jurassic one along southern margin of South China block possibly controlled by the Paleo-Tethyan closure, Cretaceous one along southern margins of North China craton, and Paleogene one in Tibetan Plateau and its margins. Orogenic gold deposits in China formed in Phanerozoic in association with various orogeny, with ore-forming ages post dating peak metamorphism. Case studies on gold districts in these belts, such as Jiaodong, Ailaoshan, and western margin of Yangtze craton, all favored the mantle fluid model.
The orogenic gold deposits show features as follows: relation to oceanic plate subduction and terrane accretion, hosted by metamorphic massif along convergent plate boundaries, controlled by ductile to brittle shear zones, low salinity and H_2 O-CO_2-CH_4 dominating ore fluid, wide formation depths varying from about 2 to 20 km and formation temperatures ranging within 200-650 ℃, temperature-dependent alteration and ore mineral assemblages. Orogenic gold deposits formed coevally to the time of cycled convergences of supercontinents. Due to the diversity of wall rock types and ore-controlling structures, ambiguity of ore geochemistry, uncertainty of fluid and metal sources and their evolutions, and disparity between source regions and ore deposition locations, two distinct origin models were proposed for orogenic gold deposits. The first is metamorphic fluid model, in which the deposits formed in prograde metamorphism of orogeny with different source from evolving regional upper crust. The auriferous fluid is considered to release from greenschist-to amphibolite-facies prograde metamorphism of upper crustal rocks,during which gold and other metals are liberated from transformation of pyrite to pyrrhotite. This model was universally applied to Phanerozoic orogenic gold deposit shosted by greenschist-facies terranes. However, it was recognized that most orogenic gold deposits formed in retrogression stage subsequent to peak metamorphism or without any spatial-temporal link to regional metamorphism, which challenged the metamorphic fluid model. Thus the mantle fluid model, which indicates that ore fluids for orogenic gold deposits are derived from devolatilization of subducted oceanic plate or fertile mantle, was proposed. Although the mantle fluid model is not compatible with the petrological diagram in phase equilibrium condition, the extensive proofs for the existence of mantle fluids and their appearance near surface support that mantle fluids are capable to transport to upper crustal levels under supercritical conditions and phase unequilibrium. The Chinese orogenic gold deposits are divided into seven gold belts: Silurian belt along Jiangnan orogen, Permian belt in Tianshan and Altay orogen, Triassic to Jurassic one along northern margin of North China craton(Solonker orogen), Triassic to Jurassic one within Paleo-Tethyan orogens, Jurassic one along southern margin of South China block possibly controlled by the Paleo-Tethyan closure, Cretaceous one along southern margins of North China craton, and Paleogene one in Tibetan Plateau and its margins. Orogenic gold deposits in China formed in Phanerozoic in association with various orogeny, with ore-forming ages post dating peak metamorphism. Case studies on gold districts in these belts, such as Jiaodong, Ailaoshan, and western margin of Yangtze craton, all favored the mantle fluid model.
引文
Andersen,T.,Neumann,E.R.,2001.Fluid Inclusions in Mantle Xenoliths.Lithos,55(1):301-320.https://doi.org/10.1016/s0024-4937(00)00049-9
Barley,M.E.,Groves,D.I.,1992.Supercontinent Cycles and the Distribution of Metal Deposits through Time.Geology,20(4):291-294.
Bath,A.B.,Walshe,J.L.,Cloutier,J.,et al.,2013.Biotite and Apatite as Tools for Tracking Pathways of Oxidized Fluids in the Archean East Repulse Gold Deposit,Australia.Economic Geology,108(4):667-690.https://doi.org/10.2113/econgeo.108.4.667
Bell,R.M.,Kolb,J.,Waight,T.E.,2018.Assessment of Lithological,Geochemical and Structural Controls on Gold Distribution in the Nalunaq Gold Deposit,South Greenland Using Three-Dimensional Implicit Modelling.Geological Society,London,Special Publications,453(1):385-405.https://doi.org/10.1144/sp453.2
Bi,X.W.,Hu,R.Z.,He,M.Y.,1997.Characteristics of OreForming Fluid of Three Gold Deposits in Ailaoshan Gold Mineralization Belt.Acta Mineralogica Sinica,17(4):435-441(in Chinese with English abstract).
Bierlein,F.P.,Crowe,D.E.,2000.Phanerozoic Orogenic Lode Gold Deposits.Reviews in Economic Geology,13:103-139.
Bierlein,F.P.,Groves,D.I.,Goldfarb,R.J.,et al.,2006.Lithospheric Controls on the Formation of Provinces Hosting Giant Orogenic Gold Deposits.Mineralium Deposita,40(8):874-886.https://doi.org/10.1007/s00126-005-0046-2
Bierlein,F.P.,Maher,S.,2001.Orogenic Disseminated Gold in Phanerozoic Fold Belts:Examples from Victoria,Australia and Elsewhere.Ore Geology Reviews,18(1-2):113-148.https://doi.org/10.1016/s0169-1368(01)00019-1
Bierlein,F.P.,Pisarevsky,S.,2008.Plume-Related Oceanic Plateaus as a Potential Source of Gold Mineralization.Economic Geology,103(2):425-430.https://doi.org/10.2113/gsecongeo.103.2.425
Blenkinsop,T.G.,Doyle,M.G.,2014.Structural Controls on Gold Mineralization on the Margin of the Yilgarn Craton,Albany-Fraser Orogen:The Tropicana Deposit,Western Australia.Journal of Structural Geology,67:189-204.https://doi.org/10.1016/j.jsg.2014.01.013
Bouchot,V.,Ledru,P.,Lerouge,C.,et al.,2005.Late Variscan Mineralizing Systems Related to Orogenic Processes:The French Massif Central.Ore Geology Reviews,27(1-4):169-197.https://doi.org/10.1016/j.oregeorev.2005.07.017
Breeding,C.M.,Ague,J.J.,2002.Slab-Derived Fluids and Quartz-Vein Formation in an Accretionary Prism,Otago Schist,New Zealand.Geology,30(6):499-502.
Browning,P.,Groves,D.I.,Blockley,J.G.,et al.,1987.Lead Isotope Constraints on the Age and Source of Gold Mineralization in the Archean Yilgarn Block,Western Australia.Economic Geology,82(4):971-986.https://doi.org/10.2113/gsecongeo.82.4.971
Bucher,K.,Grapes,R.,2011.Metamorphism of Pelitic Rocks(Metapelites).Petrogenesis of Metamorphic Rocks.Springer,Heidelberg,Berlin,257-313.
Bureau,H.,Keppler,H.,1999.Complete Miscibility between Silicate Melts and Hydrous Fluids in the Upper Mantle:Experimental Evidence and Geochemical Implications.Earth and Planetary Science Letters,165(2):187-196.https://doi.org/10.1016/s0012-821x(98)00266-0
Burnard,P.G.,Polya,D.A.,2004.Importance of Mantle Derived Fluids during Granite Associated Hydrothermal Circulation:He and Ar Isotopes of Ore Minerals from Panasqueira.Geochimica et Cosmochimica Acta,68(7):1607-1615.https://doi.org/10.1016/j.gca.2003.10.008
Cao,S.Y.,Liu,J.L.,Leiss,B.,et al.,2011.Oligo-Miocene Shearing along the Ailao Shan-Red River Shear Zone:Constraints from Structural Analysis and Zircon U/Pb Geochronology of Magmatic Rocks in the Diancang Shan Massif,SE Tibet,China.Gondwana Research,19(4):975-993.https://doi.org/10.1016/j.gr.2010.10.006
Carrier,A.,Jebrak,M.,Angelier,J.,et al.,2000.The Silidor Deposit,Rouyn-Noranda District,Abitibi Belt:Geology,Structural Evolution,and Paleostress Modeling of an Au Quartz Vein-Type Deposit in an Archean Trondhjemite.Economic Geology,95(5):1049-1065.
Chen,M.H.,Mao,J.W.,Bierlein,F.P.,et al.,2011.Structural Features and Metallogenesis of the Carlin-Type Jinfeng(Lannigou)Gold Deposit,Guizhou Province,China.Ore Geology Reviews,43(1):217-234.https://doi.org/10.1016/j.oregeorev.2011.06.009
Chen,Y.J.,Pirajno,F.,Lai,Y.,et al.,2004.Metallogenic Time and Tectonic Setting of the Jiaodong Gold Province,Eastern China.Acta Petrologica Sinica,20(4):907-922(in Chinese with English abstract).
Chen,Y.J.,Pirajno,F.,Qi,J.P.,2008.The Shanggong Gold Deposit,Eastern Qinling Orogen,China:Isotope Geochemistry and Implications for Ore Genesis.Journal of Asian Earth Sciences,33(3-4):252-266.https://doi.org/10.1016/j.jseaes.2007.12.002
Chen,Y.J.,Zhai,M.G.,Jiang,S.Y.,2009.Significant Achievements and Open Issues in Study of Orogenesis and Metallogenesis Surrounding the North China Continent.Acta Petrologica Sinica,25(11):2695-2726(in Chinese with English abstract).
Christie,A.B.,Brathwaite,R.L.,2003.Hydrothermal Alteration in Metasedimentary Rock-Hosted Orogenic Gold Deposits,Reefton Goldfield,South Island,New Zealand.Mineralium Deposita,38(1):87-107.https://doi.org/10.1007/s00126-002-0280-9
Connolly,J.A.D.,Cesare,B.,1993.C-O-H-S Fluid Composition and Oxygen Fugacity in Graphitic Metapelites.Journal of Metamorphic Geology,11(3):379-388.https://doi.org/10.1111/j.1525-1314.1993.tb00155.x
Cox,S.F.,2010.The Application of Failure Mode Diagrams for Exploring the Roles of Fluid Pressure and Stress States in Controlling Styles of Fracture-Controlled Permeability Enhancement in Faults and Shear Zones.Geofluids,10:217-233.https://doi.org/10.1111/j.1468-8123.2010.00281.x
Cox,S.F.,2016.Injection-Driven Swarm Seismicity and Permeability Enhancement:Implications for the Dynamics of Hydrothermal Ore Systems in High Fluid-Flux,OverpressuredFaulting Regimes:An Invited Paper.Economic Geology,111(3):559-587.https://doi.org/10.2113/econgeo.111.3.559
Cox,S.F.,2019.The Dynamics of Permeability Enhancement and Fluid Flow in Overpressured,Fracture Controlled Hydrothermal Systems.Economic Geology(in press).
Cox,S.F.,Etheridge,M.A.,Cas,R.A.F.,et al.,1991.Deformational Style of the Castlemaine Area,Bendigo-Ballarat Zone:Implications fore Volution of Crustal Structure in Central Victoria.Australian Journal of Earth Sciences,38(2):151-170.
Dai,J.G.,Wang,C.S.,Li,Y.L.,2012.Relicts of the Early Cretaceous Seamounts in the Central-Western Yarlung Zangbo Suture Zone,Southern Tibet.Journal of Asian Earth Sciences,53:25-37.https://doi.org/10.1016/j.jseaes.2011.12.024
Davis,G.A.,Darby,B.J.,Zheng,Y.D.,et al.,2002.Geometric and Temporal Evolution of an Extensional Detachment Fault,Hohhot Metamorphic Core Complex,Inner Mongolia,China.Geology,30(11):1003-1006.
De Boorder,H.,2012.Spatial and Temporal Distribution of the Orogenic Gold Deposits in the Late Palaeozoic Variscides and Southern Tianshan:How Orogenic are They?Ore Geology Reviews,46:1-31.https://doi.org/10.1016/j.oregeorev.2012.01.002
Deng,J.,Liu,X.F.,Wang,Q.F.,et al.,2015a.Origin of the Jiaodong-Type Xinli Gold Deposit,Jiaodong Peninsula,China:Constraints from Fluid Inclusion and C-D-O-S-Sr Isotope Compositions.Ore Geology Reviews,65:674-686.https://doi.org/10.1016/j.oregeorev.2014.04.018
Deng,J.,Wang,Q.F.,Li,G.J.,et al.,2015b.Structural Control and Genesis of the Oligocene Zhenyuan Orogenic Gold Deposit,SW China.Ore Geology Reviews,65:42-54.https://doi.org/10.1016/j.oregeorev.2014.08.002
Deng,J.,Wang,C.M.,Bagas,L.,et al.,2015c.Cretaceous-Cenozoic Tectonic History of the Jiaojia Fault and Gold Mineralization in the Jiaodong Peninsula,China:Constraints from Zircon U-Pb,Illite K-Ar,and Apatite Fission Track Thermochronometry.Mineralium Deposita,50(8):987-1006.https://doi.org/10.1007/s00126-015-0584-1
Deng,J.,Wang,Q.F.,2016.Gold Mineralization in China:Metallogenic Provinces,Deposit Types and Tectonic Framework.Gondwana Research,36:219-274.https://doi.org/10.1016/j.gr.2015.10.003
Deng,J.,Wang,Q.F.,Li,G.J.,et al.,2014a.Tethys Tectonic Evolution and Its Bearing on the Distribution of Important Mineral Deposits in the Sanjiang Region,SW China.Gondwana Research,26(2):419-437.https://doi.org/10.1016/j.gr.2013.08.002
Deng,J.,Wang,Q.F.,Li,G.J.,et al.,2014b.CenozoicTectono-Magmatic and Metallogenic Processes in the Sanjiang Region,Southwestern China.Earth-Science Reviews,138:268-299.https://doi.org/10.1016/j.earscirev.2014.05.015
Deng,J.,Yuan,W.M.,Carranza,E.J.M.,et al.,2014c.Geochronology and Thermochronometry of the Jiapigou Gold Belt,Northeastern China:New Evidence for Multiple Episodes of Mineralization.Journal of Asian Earth Sciences,89:10-27.
Deng,J.,Wang,Q.F.,Wan,L.,et al.,2009a.Self-Similar Fractal Analysis of Gold Mineralization of Dayingezhuang Disseminated-Veinlet Deposit in Jiaodong Gold Province,China.Journal of Geochemical Exploration,102(2):95-102.
Deng,J.,Yang,L.Q.,Gao,B.F.,et al.,2009b.Fluid Evolution and Metallogenic Dynamics during Tectonic Regime Transition:Example from the Jiapigou Gold Belt in Northeast China.Resource Geology,59(2):140-152.https://doi.org/10.1111/j.1751-3928.2009.00086.x
Deng,J.,Wang,Q.F.,Wan,L.,et al.,2011.A Multifractal Analysis of Mineralization Characteristics of the Dayingezhuang Disseminated-Veinlet Gold Deposit in the Jiaodong Gold Province of China.Ore Geology Reviews,40(1):54-64.
Deng,J.,Wang,Q.F.,Yang,L.Q.,et al.,2010a.Delineation and Explanation of Geochemical Anomalies Using Fractal Models in the Heqing Area,Yunnan Province,China.Journal of Geochemical Exploration,105(3):95-105.https://doi.org/10.1016/j.gexplo.2010.04.005
Deng,J.,Yang,L.Q.,Sun,Z.S.,et al.,2010b.A Metallogenic Model of Gold Deposits of the Jiaodong Granite-Greenstone Belt.Acta Geologica Sinica(English Edition),77(4):537-546.
Deng,J.,Yang,L.Q.,Wang,C.M.,2011.Research Advances of Superimposed Orogenesis and Metallogenesis in the Sanjiang Tethys.Acta Petrologica Sinica,27(9):2501-2509(in Chinese with English abstract).
Ding,Q.F.,Jiang,S.Y.,Sun,F.Y.,2014.Zircon U-Pb Geochronology,Geochemical and Sr-Nd-Hf Isotopic Compositions of the Triassic Granite and Diorite Dikes from the Wulonggou Mining Area in the Eastern Kunlun Orogen,NW China:Petrogenesis and Tectonic Implications.Lithos,205:266-283.https://doi.org/10.1016/j.lithos.2014.07.015
Drummond,B.J.,Goleby,B.R.,Swager,C.P.,et al.,1993.Constraints on Archean Crustal Composition and Structure Provided by Deep Seismic Sounding in the Yilgarn Block.Ore Geology Reviews,8(1-2):117-124.
Du,J.X.,Zhang,L.F.,Bader,T.,et al.,2014.Metamorphic Evolution of Ultrahigh-Pressure Rocks from Chinese Southwestern Tianshan and a Possible Indicator of UHP-Metamorphism Using Garnet Composition in Low-TEclogites.Journal of Asian Earth Sciences,91:69-88.https://doi.org/10.1016/j.jseaes.2014.04.010
Dziggel,A.,Poujol,M.,Otto,A.,et al.,2010.New U-Pb and40Ar/39Ar Ages from the Northern Margin of the Barberton Greenstone Belt,South Africa:Implications for the Formation of Mesoarchaean Gold Deposits.Precambrian Research,179(1-4):206-220.https://doi.org/10.1016/j.precamres.2010.03.006
Eisenlohr,B.N.,Groves,D.I.,Partington,G.A.,1989.CrustalScale Shear Zones and Their Significance to Archaean Gold Mineralization in Western Australia.Mineralium Deposita,24(1):1-8.
Elmer,F.L.,White,R.W.,Powell,R.,2006.Devolatilization of Metabasic Rocks during Greenschist-Amphibolite Facies Metamorphism.Journal of Metamorphic Geology,24(6):497-513.https://doi.org/10.1111/j.1525-1314.2006.00650.x
Evans,K.A.,2010.A Test of the Viability of Fluid-Wall Rock Interaction Mechanisms for Changes in Opaque Phase Assemblage in Metasedimentary Rocks in the Kambalda-St.Ives Goldfield,Western Australia.Mineralium Deposita,45(2):207-213.
Evans,K.A.,Phillips,G.N.,Powell,R.,2006.Rock-Buffering of Auriferous Fluids in Altered Rocks Associated with the Golden Mile-Style Mineralization,Kalgoorlie Gold Field,Western Australia.Economic Geology,101(4):805-817.https://doi.org/10.2113/gsecongeo.101.4.805
Fan,H.R.,Zhai,M.G.,Xie,Y.H.,et al.,2003.Ore-Forming Fluids Associated with Granite-Hosted Gold Mineralization at the Sanshandao Deposit,Jiaodong Gold Province,China.Mineralium Deposita,38(6):739-750.https://doi.org/10.1007/s00126-003-0368-x
Finch,E.G.,Tomkins,A.G.,2017.Pyrite-Pyrrhotite Stability in a Metamorphic Aureole:Implications for Orogenic Gold Genesis.Economic Geology,112(3):661-674.https://doi.org/10.2113/econgeo.112.3.661
Finlay,A.J.,Selby,D.,Osborne,M.J.,et al.,2010.FaultCharged Mantle-Fluid Contamination of United Kingdom North Sea Oils:Insights from Re-Os Isotopes.Geology,38(11):979-982.https://doi.org/10.1130/g31201.1
Fridovsky,V.Y.,2017.Structural Control of Orogenic Gold Deposits of the Verkhoyansk-Kolyma Folded Region,Northeast Russia.Ore Geology Reviews,103:38-55.https://doi.org/10.1016/j.oregeorev.2017.01.006
Fu,B.,Touret,J.L.R.,2014.From Granulite Fluids to QuartzCarbonate Megashear Zones:The Gold Rush.Geoscience Frontiers,5(5):747-758.https://doi.org/10.1016/j.gsf.2014.03.013
Gao,L.,Wang,Q.F.,Deng,J.,et al.,2018.Relationship between Orogenic Gold Mineralization and Crustal Shearing along Ailaoshan-Red River Belt,Southeastern Tibetan Plateau:New Constraint from Paleomagnetism.Geochemistry,Geophysics,Geosystems,19(7):2225-2242.https://doi.org/10.1029/2018gc007493
Gebre-Mariam,M.,Hagemann,S.G.,Groves,D.I.,1995.AClassification Scheme for Epigenetic Archaean LodeGold Deposits.Mineralium Deposita,30(5):408-410.
Goldfarb,R.J.,Baker,T.,Dube,B.,et al.,2005.Distribution,Character,and Genesis of Gold Deposits in Metamorphic Belts.In:Hedenquist,J.W.,Thompson,J.F.H.,Goldfarb,J.,eds.,Economic Geology 100th Anniversary Volume.Society of Economic Geologists,Littleton,Colorado,USA,407-450.
Goldfarb,R.J.,Groves,D.I.,2015.Orogenic Gold:Common or Evolving Fluid and Metal Sources through Time.Lithos,233:2-26.https://doi.org/10.1016/j.lithos.2015.07.011
Goldfarb,R.J.,Groves,D.I.,Gardoll,S.,2001.Orogenic Gold and Geologic Time:A Global Synthesis.Ore Geology Reviews,18(1-2):1-75.https://doi.org/10.1016/s0169-1368(01)00016-6
Goldfarb,R.J.,Hart,C.,Davis,G.,et al.,2007.East Asian Gold:Deciphering the Anomaly of Phanerozoic Gold in Precambrian Cratons.Economic Geology,102(3):341-345.https://doi.org/10.2113/gsecongeo.102.3.341
Goldfarb,R.J.,Santosh,M.,2014.The Dilemma of the Jiaodong Gold Deposits:Are They Unique?Geoscience Frontiers,5(2):139-153.https://doi.org/10.1016/j.gsf.2013.11.001
Griffin,W.L.,Begg,G.C.,O'Reilly,S.Y.,2013.ContinentalRoot Control on the Genesis of Magmatic Ore Deposits.Nature Geoscience,6(11):905-910.https://doi.org/10.1038/ngeo1954
Groves,D.,Barnicoat,A.C.,Barley,M.,et al.,1992.SubGreenschist to Granulite-Hosted Archaean Lode-Gold Deposits of the Yilgarn Craton:A Depositional Continuum from Deep-Sourced Hydrothermal Fluids in Crustalscale Plumbing Systems.Geology Department(Key Centre)and University Extension.The University of Western Australia Publication,Perth,Australia,325-338.
Groves,D.I.,1993.The Crustal Continuum Model for LateArchaean Lode-Gold Deposits of the Yilgarn Block,Western Australia.Mineralium Deposita,28(6):366-374.
Groves,D.I.,Condie,K.C.,Goldfarb,R.J.,et al.,2005.100th Anniversary Special Paper:Secular Changes in Global Tectonic Processes and Their Influence on the Temporal Distribution of Gold-Bearing Mineral Deposits.Economic Geology,100(2):203-224.https://doi.org/10.2113/gsecongeo.100.2.203
Groves,D.I.,Goldfarb,R.J.,Gebre-Mariam,M.,et al.,1998.Orogenic Gold Deposits:A Proposed Classification in the Context of Their Crustal Distribution and Relationship to Other Gold Deposit Types.Ore Geology Reviews,13(1-5):7-27.https://doi.org/10.1016/s0169-1368(97)00012-7
Groves,D.I.,Goldfarb,R.J.,Robert,F.,et al.,2003.Gold Deposits in Metamorphic Belts:Overview of Current Understanding,Outstanding Problems,Future Research,and Exploration Significance.Economic Geology,98(1):1-29.https://doi.org/10.2113/gsecongeo.98.1.1
Groves,D.I.,Santosh,M.,2015.Province-Scale Commonalities of Some World-Class Gold Deposits:Implications for Mineral Exploration.Geoscience Frontiers,6(3):389-399.https://doi.org/10.1016/j.gsf.2014.12.007
Groves,D.I.,Santosh,M.,2016.The Giant Jiaodong Gold Province:The Key to a Unified Model for Orogenic Gold Deposits?Geoscience Frontiers,7(3):409-417.
Groves,D.I.,Santosh,M.,Deng,J.,et al.,2019.A Holistic Model for the Origin of Orogenic Gold Deposits and Its Implications for Exploration.Mineralium Deposita.https://doi.org/10.1007/s00126-019-0087-5.
Groves,D.I.,Santosh,M.,Goldfarb,R.J.,et al.,2018.Structural Geometry of Orogenic Gold Deposits:Implications for Exploration of World-Class and Giant Deposits.Geoscience Frontiers,9(4):1163-1177.
Gumiel,P.,Sanderson,D.J.,Arias,M.,et al.,2010.Analysis of the Fractal Clustering of Ore Deposits in the Spanish Iberian Pyrite Belt.Ore Geology Reviews,38(4):307-318.https://doi.org/10.1016/j.oregeorev.2010.08.001
Guo,Z.F.,Wilson,M.,Zhang,M.L.,et al.,2013.Post-Collisional,K-Rich Mafic Magmatism in South Tibet:Constraints on Indian Slab-to-Wedge Transport Processes and Plateau Uplift.Contributions to Mineralogy and Petrology,165(6):1311-1340.https://doi.org/10.1007/s00410-013-0860-y
Haddad-Martim,P.M.,Carranza,E.J.M.,de Souza Filho,C.R.,2018.The Fractal Nature of Structural Controls on Ore Formation:The Case of the Iron Oxide Copper-Gold Deposits in the Carajás Mineral Province,Brazilian Amazon.Economic Geology,113(7):1499-1524.https://doi.org/10.5382/econgeo.2018.4600
Harrison,T.M.,Yin,A.,Grove,M.,et al.,2000.The Zedong Window:A Record of Superposed Tertiary Convergence in Southeastern Tibet.Journal of Geophysical Research:Solid Earth,105(B8):19211-19230.https://doi.org/10.1029/2000jb900078
Hart,C.,2005.Classifying,Distinguishing and Exploring for Intrusion-Related Gold Systems.The Gangue,87(1):9.
Helt,K.M.,Williams-Jones,A.E.,Clark,J.R.,et al.,2014.Constraints on the Genesis of the Archean Oxidized,Intrusion-Related Canadian Malartic Gold Deposit,Quebec,Canada.Economic Geology,109(3):713-735.https://doi.org/10.2113/econgeo.109.3.713
Hodkiewicz,P.F.,Groves,D.I.,Davidson,G.J.,et al.,2009.Influence of Structural Setting on Sulphur Isotopes in Archean Orogenic Gold Deposits,Eastern Goldfields Province,Yilgarn,Western Australia.Mineralium Deposita,44(2):129-150.https://doi.org/10.1007/s00126-008-0211-5
Hou,Z.Q.,Cook,N.J.,2009.Metallogenesis of the Tibetan Collisional Orogen:A Review and Introduction to the Special Issue.Ore Geology Reviews,36(1-3):2-24.https://doi.org/10.1016/j.oregeorev.2009.05.001
Hou,Z.Q.,Duan,L.F.,Lu,Y.J.,et al.,2015.Lithospheric Architecture of the Lhasa Terrane and Its Control on Ore Deposits in the Himalayan-Tibetan Orogen.Economic Geology,110(6):1541-1575.https://doi.org/10.2113/econgeo.110.6.1541
Hou,Z.Q.,Zaw,K.,Pan,G.T.,et al.,2007.Sanjiang Tethyan Metallogenesis in S.W.China:Tectonic Setting,Metallogenic Epochs and Deposit Types.Ore Geology Reviews,31(1-4):48-87.https://doi.org/10.1016/j.oregeorv.2004.12.007
Hronsky,J.M.A.,Groves,D.I.,Loucks,R.R.,et al.,2012.AUnified Model for Gold Mineralisation in Accretionary Orogens and Implications for Regional-Scale Exploration Targeting Methods.Mineralium Deposita,47(4):339-358.https://doi.org/10.1007/s00126-012-0402-y
Hyndman,R.D.,McCrory,P.A.,Wech,A.,et al.,2015.Cascadia Subducting Plate Fluids Channelled to Fore-ArcMantle Corner:ETS and Silica Deposition.Journal of Geophysical Research:Solid Earth,120(6):4344-4358.https://doi.org/10.1002/2015jb011920
Jia,S.S.,Wang,E.D.,Fu,J.F.,et al.,2018.Indosinian Gold Mineralization and Magmatic-Hydrothermal Evolution of the Hadamengou Gold Deposit at the Northern Margin of the North China Craton:Constraints from K-Feldspar Laser40Ar/39Ar Dating.Journal of Geochemical Exploration,190:314-324.https://doi.org/10.1016/j.gexplo.2018.04.002
Jiang,S.H.,Nie,F.J.,Hu,P.,et al.,2009.Mayum:An Orogenic Gold Deposit in Tibet,China.Ore Geology Reviews,36(1-3):160-173.https://doi.org/10.1016/j.oregeorev.2009.03.006
Katayama,I.,Terada,T.,Okazaki,K.,et al.,2012.Episodic Tremor and Slow Slip Potentially Linked to Permeability Contrasts at the Moho.Nature Geoscience,5(10):731-734.https://doi.org/10.1038/ngeo1559
Kawano,S.,Katayama,I.,Okazaki,K.,2011.Permeability Anisotropy of Serpentinite and Fluid Pathways in a Subduction Zone.Geology,39(10):939-942.https://doi.org/10.1130/g32173.1
Kennedy,B.M.,1997.Mantle Fluids in the San Andreas Fault System,California.Science,278(5341):1278-1281.
Kennedy,B.M.,van Soest,M.C.,2007.Flow of Mantle Fluids through the Ductile Lower Crust:Helium Isotope Trends.Science,318(5855):1433-1436.
Kerrich,R.,Fyfe,W.S.,1981.The Gold:Carbonate Association,Source of CO2,and CO2Fixation Reactions in Archaean Lode Deposits.Chemical Geology,33(1-4):265-294.
Kerrich,R.,Goldfarb,R.,Groves,D.,et al.,2000.The Characteristics,Origins,and Geodynamic Settings of Supergiant Gold Metallogenic Provinces.Science in China(Series D),43(Suppl.1):1-68.
Kerrich,R.,Wyman,D.,1990.Geodynamic Setting of Mesothermal Gold Deposits:An Association with Accretionary Tectonic Regimes.Geology,18(9):882-825.
Klein-Ben David,O.,Pettke,T.,Kessel,R.,2011.Chromium Mobility in Hydrous Fluids at Upper Mantle Conditions.Lithos,125(1-2):122-130.
Klemperer,S.L.,Kennedy,B.M.,Sastry,S.R.,et al.,2013.Mantle Fluids in the Karakoram Fault:Helium Isotope Evidence.Earth and Planetary Science Letters,366:59-70.https://doi.org/10.1016/j.epsl.2013.01.013
Knight,J.T.,Groves,D.I.,Ridley,J.R.,1993.The Coolgardie Goldfied,Western Australia:District-Scale Controls on an Archaean Gold Camp in an Amphibolite Facies Terrane.Mineralium Deposita,28(6):436-456.
Knight,J.T.,Ridley,J.R.,Groves,D.I.,2000.The Archean Amphibolite Facies Coolgardie Goldfield,Yilgarn Craton,Western Australia:Nature,Controls,and Gold FieldScale Patterns of Hydrothermal Wall-Rock Alteration.Economic Geology,95(1):49-84.https://doi.org/10.2113/gsecongeo.95.1.49
Kolb,J.,Dziggel,A.,Bagas,L.,2015.Hypozonal Lode Gold Deposits:A Genetic Concept Based on a Review of the New Consort,Renco,Hutti,Hira Buddini,Navachab,Nevoria and the Granites Deposits.Precambrian Research,262:20-44.https://doi.org/10.1016/j.precamres.2015.02.022
Kolb,J.,Kisters,A.F.M.,Hoernes,S.,et al.,2000.The Origin of Fluids and Nature of Fluid-Rock Interaction in MidCrustal Auriferous Mylonites of the Renco Mine,Southern Zimbabwe.Mineralium Deposita,35(2-3):109-125.https://doi.org/10.1007/s001260050010
Kolb,J.,Meyer,M.F.,2002.Fluid Inclusion Record of the Hypozonal Orogenic Renco Gold Deposit(Zimbabwe)during the Retrograde P-T Evolution.Contributions to Mineralogy and Petrology,143(4):495-509.https://doi.org/10.1007/s00410-002-0360-y
Kolb,J.,Rogers,A.,Meyer,F.M.,2005.Relative Timing of Deformation and Two-Stage Gold Mineralization at the Hutti Mine,Dharwar Craton,India.Mineralium Deposita,40(2):156-174.
Kontak,D.J.,Smith,P.K.,Kerrich,R.,et al.,1990.Integrated Model for Meguma Group Lode Gold Deposits,Nova Scotia,Canada.Geology,18(3):238-242.
LaFlamme,C.,Jamieson,J.W.,Fiorentini,M.L.,et al.,2018.Investigating Sulfur Pathways through the Lithosphere by Tracing Mass Independent Fractionation of Sulfur to the Lady Bountiful Orogenic Gold Deposit,Yilgarn Craton.Gondwana Research,58:27-38.https://doi.org/10.1016/j.gr.2018.02.005
Large,R.R.,Bull,S.W.,Maslennikov,V.V.,2011.A Carbonaceous Sedimentary Source-Rock Model for CarlinType and Orogenic Gold Deposits.Economic Geology,106(3):331-358.https://doi.org/10.2113/econgeo.106.3.331
Large,R.R.,Danyushevsky,L.,Hollit,C.,et al.,2009.Gold and Trace Element Zonation in Pyrite Using a Laser Imaging Technique:Implications for the Timing of Gold in Orogenic and Carlin-Style Sediment-Hosted Deposits.Economic Geology,104(5):635-668.https://doi.org/10.2113/gsecongeo.104.5.635
Large,R.R.,Maslennikov,V.V.,Robert,F.,et al.,2007.Multistage Sedimentary and Metamorphic Origin of Pyrite and Gold in the Giant Sukhoi Log Deposit,Lena Gold Province,Russia.Economic Geology,102(7):1233-1267.https://doi.org/10.2113/gsecongeo.102.7.1233
Lawrence,D.M.,Treloar,P.J.,Rankin,A.H.,et al.,2013.The Geology and Mineralogy of the Loulo Mining District,Mali,West Africa:Evidence for Two Distinct Styles of Orogenic Gold Mineralization.Economic Geology,108(2):199-227.https://doi.org/10.2113/econgeo.108.2.199
Lebrun,E.,Miller,J.,Thébaud,N.,et al.,2017.Structural Controls on an Orogenic Gold System:The World-Class Siguiri Gold District,Siguiri Basin,Guinea,West Africa.Economic Geology,112(1):73-98.https://doi.org/10.2113/econgeo.112.1.73
Li,H.J.,Wang,Q.F.,Deng,J.,et al.,2019a.Alteration and Mineralization Styles of the Orogenic Disseminated Zhenyuan Gold Deposit,Southeastern Tibet:Contrast with Carlin Gold Deposit.Geoscience Frontiers.https://doi.org/10.1016/j.gsf.2019.01.008
Li,H.J.,Wang,Q.F.,Groves,D.I.,et al.,2019b.Alteration of Eocene Lamprophyres in the Zhenyuan Orogenic Gold Deposit,Yunnan Province,China:Composition and Evolution of Ore Fluids.Ore Geology Reviews,107:1068-1083.https://doi.org/10.1016/j.oregeorev.2019.03.032
Li,H.J.,Wang,Q.F.,Yang,L.,et al.,2017.Orogenic Gold Deposits Formed in Tibetan Collisional Orogen Setting:Geotectonic Setting,Geological and Geochemical Features.Acta Petrologica Sinica,33(7):2189-2201(in Chinese with English abstract).
Li,J.F.,Xia,B.,Liu,L.W.,et al.,2009.SHRIMP U-Pb Dating for the Gabbro in Qunrang Ophiolite,Tibet:The Geochronology Constraint for the Development of Eastern Tethys Basin.Geotectonica et Metallogenia,33(2):294-298.
Li,J.W.,Bi,S.J.,Selby,D.,et al.,2012a.Giant Mesozoic Gold Provinces Related to the Destruction of the North China Craton.Earth and Planetary Science Letters,349-350:26-37.https://doi.org/10.1016/j.epsl.2012.06.058
Li,J.W.,Li,Z.K.,Zhou,M.F.,et al.,2012b.The Early Cretaceous Yangzhaiyu Lode Gold Deposit,North China Craton:A Link between Craton Reactivation and Gold Veining.Economic Geology,107(1):43-79.
Li,J.W.,Vasconcelos,P.M.,Zhou,M.F.,et al.,2006.Geochronology of the Pengjiakuang and Rushan Gold Deposits,Eastern Jiaodong Gold Province,Northeastern China:Implications for Regional Mineralization and Geodynamic Setting.Economic Geology,101(5):1023-1038.https://doi.org/10.2113/gsecongeo.101.5.1023
Li,L.,Santosh,M.,Li,S.R.,2015.The‘Jiaodong Type’Gold Deposits:Characteristics,Origin and Prospecting.Ore Geology Reviews,65:589-611.https://doi.org/10.1016/j.oregeorev.2014.06.021
Li,Q.L.,Chen,F.K.,Yang,J.H.,et al.,2008.Single Grain Pyrite Rb-Sr Dating of the Linglong Gold Deposit,Eastern China.Ore Geology Reviews,34(3):263-270.https://doi.org/10.1016/j.oregeorev.2007.10.003
Li,S.H.,Zhang,J.,Deng,J.,et al.,2011.The Characteristics of Ore-Forming Fluid and Genetic Type of the Chang'an Gold Deposit in Southern Ailaoshan Metallogenic Belt.Acta Petrologica Sinica,27(12):3777-3786(in Chinese with English abstract).
Li,X.F.,Mao,J.W.,Wang,C.Z.,et al.,2007.The Daduhe Gold Field at the Eastern Margin of the Tibetan Plateau:He,Ar,S,O,and H Isotopic Data and Their Metallogenic Implications.Ore Geology Reviews,30(3-4):244-256.https://doi.org/10.1016/j.oregeorev.2005.10.005
Liang,Y.H.,Sun,X.M.,Shi,G.Y.,et al.,2011.Ore-Forming Fluid Geochemistry and Genesis of Laowangzhai Large Scale Orogenic Gold Deposit in Ailaoshan Gold Belt,Yunnan Province,China.Acta Petrologica Sinica,27(9):2533-2540(in Chinese with English abstract).
Lin,T.H.,Chung,S.L.,Chiu,H.Y.,et al.,2012.Zircon U-Pb and Hf Isotope Constraints from the Ailao Shan-Red River Shear Zone on the Tectonic and Crustal Evolution of Southwestern China.Chemical Geology,291(1):23-37.https://doi.org/10.1016/j.chemgeo.2011.11.011
Liu,J.J.,Liu,C.H.,Carranza,E.J.M.,et al.,2015a.Geological Characteristics and Ore-Forming Process of the Gold Deposits in the Western Qinling Region,China.Journal of Asian Earth Sciences,103:40-69.https://doi.org/10.1016/j.jseaes.2014.11.012
Liu,H.C.,Wang,Y.J.,Cawood,P.A.,et al.,2015b.Record of Tethyan Ocean Closure and Indosinian Collision along the Ailaoshan Suture Zone(SW China).Gondwana Research,27(3):1292-1306.https://doi.org/10.1016/j.gr.2013.12.013
Liu,W.,Fei,P.X.,2006.Methane-Rich Fluid Inclusions from Ophiolitic Dunite and Post-Collisional Mafic-Ultramafic Intrusion:The Mantle Dynamics underneath the PalaeoAsian Ocean through to the Post-Collisional Period.Earth and Planetary Science Letters,242(3-4):286-301.https://doi.org/10.1016/j.epsl.2005.11.059
MacKenzie,D.J.,Craw,D.,Begbie,M.,2007.Mineralogy,Geochemistry,and Structural Controls of a Disseminated Gold-Bearing Alteration Halo around the Schist-Hosted Bullendale Orogenic Gold Deposit,New Zealand.Journal of Geochemical Exploration,93(3):160-176.
Malpas,J.,Zhou,M.F.,Robinson,P.T.,et al.,2003.Geochemical and Geochronological Constraints on the Origin and Emplacement of the Yarlung Zangbo Ophiolites,Southern Tibet.Geological Society,London,Special Publications,218(1):191-206.https://doi.org/10.1144/gsl.sp.2003.218.01.11
Mao,J.W.,Pirajno,F.,Xiang,J.F.,et al.,2011.Mesozoic Molybdenum Deposits in the East Qinling-Dabie Orogenic Belt:Characteristics and Tectonic Settings.Ore Geology Reviews,43(1):264-293.https://doi.org/10.1016/j.oregeorev.2011.07.009
Mao,J.W.,Qiu,Y.M.,Goldfarb,R.J.,et al.,2002.Geology,Distribution,and Classification of Gold Deposits in the Western Qinling Belt,Central China.Mineralium Deposita,37(3-4):352-377.
Mao,J.W.,Wang,Y.T.,Li,H.M.,et al.,2008.The Relationship of Mantle-Derived Fluids to Gold Metallogenesis in the Jiaodong Peninsula:Evidence from D-O-C-S Isotope Systematics.Ore Geology Reviews,33(3-4):361-381.https://doi.org/10.1016/j.oregeorev.2007.01.003
Mao,J.W.,Xie,G.Q.,Li,X.F.,et al.,2004.Mesozoic Large Scale Mineralization and Multiple Lithospheric Extension in South China.Earth Science Frontiers,11(1):45-55(in Chinese with English abstract).
Mao,J.W.,Xie,G.Q.,Zhang,Z.H.,et al.,2005.Mesozoic Large-Scale Metallogenic Pulses in North China and Corresponding Geodynamic Settings.Acta Petrologica Sinica,21(1):169-188(in Chinese with English abstract).
McNaughton,N.J.,Groves,D.I.,Witt,W.K.,1993.The Source of Lead in Archaean Lode Gold Deposits of the Menzies-Kalgoorlie-Kambalda Region,Yilgarn Block,Western Australia.Mineralium Deposita,28(6):495-502.
Mernagh,T.P.,Bierlein,F.P.,2008.Transport and Precipitation of Gold in Phanerozoic Metamorphic Terranes from Chemical Modeling of Fluid-Rock Interaction.Economic Geology,103(8):1613-1640.https://doi.org/10.2113/gsecongeo.103.8.1613
Morelli,R.,Creaser,R.A.,Seltmann,R.,et al.,2007.Age and Source Constraints for the Giant Muruntau Gold Deposit,Uzbekistan,from Coupled Re-Os-He Isotopes in Arsenopyrite.Geology,35(9):795-798.
Müller,D.,Groves,D.I.,1997.Indirect Associations between Lamprophyres and Gold-Copper Deposits.In:Müller,D.,Groves,D.I.,eds.,Potassic Igneous Rocks and Associated Gold-Copper Mineralization.Springer,Berlin,Heidelberg,143-166.
Munro,M.A.,Ord,A.,Hobbs,B.E.,2018.Spatial Organization of Gold and Alteration Mineralogy in Hydrothermal Systems:Wavelet Analysis of Drillcore from Sunrise Dam Gold Mine,Western Australia.Geological Society,London,Special Publications,453(1):165-204.https://doi.org/10.1144/sp453.10
Nesbitt,B.E.,1991.Phanerozoic Gold Deposits in Tectonically Active Continental Margins.In:Nesbitt,B.E.,ed.,Gold Metallogeny and Exploration.Springer,Boston,MA,104-132.
Peacock,S.A.,1990.Fluid Processes in Subduction Zones.Science,248(4953):329-337.https://doi.org/10.1126/science.248.4953.329
Peacock,S.M.,Christensen,N.I.,Bostock,M.G.,et al.,2011.High Pore Pressures and Porosity at 35 km Depth in the Cascadia Subduction Zone.Geology,39(5):471-474.https://doi.org/10.1130/g31649.1
Phillips,G.N.,Powell,R.,1993.Link between Gold Provinces.Economic Geology,88(5):1084-1098.https://doi.org/10.2113/gsecongeo.88.5.1084
Phillips,G.N.,Powell,R.,2009.Formation of Gold Deposits:Review and Evaluation of the Continuum Model.EarthScience Reviews,94(1-4):1-21.https://doi.org/10.1016/j.earscirev.2009.02.002
Phillips,G.N.,Powell,R.,2010.Formation of Gold Deposits:A Metamorphic Devolatilization Model.Journal of Metamorphic Geology,28(6):689-718.
Phillips,G.N.,Powell,R.,2015.A Practical Classification of Gold Deposits,with a Theoretical Basis.Ore Geology Reviews,65:568-573.https://doi.org/10.1016/j.oregeorev.2014.04.006
Pili,é.,Kennedy,B.M.,Conrad,M.E.,et al.,2011.Isotopic Evidence for the Infiltration of Mantle and Metamorphic CO2-H2O Fluids from below in Faulted Rocks from the San Andreas Fault System.Chemical Geology,281(3-4):242-252.https://doi.org/10.1016/j.chemgeo.2010.12.011
Pitcairn,I.K.,Craw,D.,Teagle,D.A.H.,2015.Metabasalts as Sources of Metals in Orogenic Gold Deposits.Mineralium Deposita,50(3):373-390.doi:10.1007/s00126-014-0547-y
Pitcairn,I.K.,Teagle,D.A.H.,Craw,D.,et al.,2006.Sources of Metals and Fluids in Orogenic Gold Deposits:Insights from the Otago and Alpine Schists,New Zealand.Economic Geology,101(8):1525-1546.https://doi.org/10.2113/gsecongeo.101.8.1525
Ridley,J.R.,Diamond,L.W.,2000.Fluid Chemistry of Orogenic Lode Gold Deposits and Implications for Genetic Models.Reviews in Economic Geology,13:141-162.
Romer,R.L.,Kroner,U.,2018.Paleozoic Gold in the Appalachians and Variscides.Ore Geology Reviews,92:475-505.https://doi.org/10.1016/j.oregeorev.2017.11.021
Rospabé,M.,Ceuleneer,G.,Benoit,M.,et al.,2017.Origin of the Dunitic Mantle-Crust Transition Zone in the Oman Ophiolite:The Interplay between Percolating Magmas and High-Temperature Hydrous Fluids.Geology,45(5):471-474.https://doi.org/10.1130/g38778.1
Saager,R.,Meyer,M.,Muff,R.,1982.Gold Distribution in Supracrustal Rocks from Archean Greenstone Belts of Southern Africa and from Paleozoic Ultramafic Complexes of the European Alps;Metallogenic and Geochemical Implications.Economic Geology,77(1):1-24.https://doi.org/10.2113/gsecongeo.77.1.1
Sack,P.J.,Large,R.R.,Gregory,D.D.,2018.Geochemistry of Shale and Sedimentary Pyrite as a Proxy for Gold Fertility in the Selwyn Basin Area,Yukon.Mineralium Deposita,53(7):997-1018.https://doi.org/10.1007/s00126-018-0793-5
Safonov,Y.G.,2010.Topical Issues of the Theory of Gold Deposit Formation.Geology of Ore Deposits,52(6):438-458.
Sarma,D.S.,Fletcher,I.R.,Rasmussen,B.,et al.,2011.Archaean Gold Mineralization Synchronous with Late Cratonization of the Western Dharwar Craton,India:2.52 Ga U-Pb Ages of Hydrothermal Monazite and Xenotime in Gold Deposits.Mineralium Deposita,46(3):273-288.
Sausse,J.,Jacquot,E.,Fritz,B.,et al.,2001.Evolution of Crack Permeability during Fluid-Rock Interaction.Example of the Brézouard Granite(Vosges,France).Tectonophysics,336(1-4):199-214.https://doi.org/10.1016/s0040-1951(01)00102-0
Schrauder,M.,Navon,O.,1994.Hydrous and Carbonatitic Mantle Fluids in Fibrous Diamonds from Jwaneng,Botswana.Geochimica et Cosmochimica Acta,58(2):761-771.https://doi.org/10.1016/0016-7037(94)90504-5
Selvaraja,V.,Caruso,S.,Fiorentini,M.L.,et al.,2017.Atmospheric Sulfur in the Orogenic Gold Deposits of the Archean Yilgarn Craton,Australia.Geology,45(8):691-694.
Seno,T.,Kirby,S.H.,2014.Formation of Plate Boundaries:The Role of Mantle Volatilization.Earth-Science Reviews,129:85-99.https://doi.org/10.1016/j.earsciev.2013.10.011
Sibson,R.H.,1996.Structural Permeability of Fluid-Driven Fault-Fracture Meshes.Journal of Structural Geology,18(8):1031-1042.https://doi.org/10.1016/0191-8141(96)00032-6
Sibson,R.H.,2001.Seismogenic Framework for Ore Deposition.Reviews in Economic Geology,14:25-50.
Sibson,R.H.,2004.Controls on Maximum Fluid Overpressure Defining Conditions for Mesozonal Mineralisation.Journal of Structural Geology,26(6-7):1127-1136.https://doi.org/10.1016/j.jsg.2003.11.003
Sibson,R.H.,2013.Stress Switching in Subduction Forearcs:Implications for Overpressure Containment and Strength Cycling on Megathrusts.Tectonophysics,600:142-152.https://doi.org/10.1016/j.tecto.2013.02.035
Sibson,R.H.,Robert,F.,Poulsen,K.H.,1988.High-Angle Reverse Faults,Fluid-Pressure Cycling,and Mesothermal Gold-Quartz Deposits.Geology,16(6):551-555.
Sibson,R.H.,Scott,J.,1998.Stress/Fault Controls on the Containment and Release of Overpressured Fluids:Examples from Gold-Quartz Vein Systems in Juneau,Alaska;Victoria,Australia and Otago,New Zealand.Ore Geology Reviews,13(1-5):293-306.https://doi.org/10.1016/s0169-1368(97)00023-1
Sillitoe,R.H.,1991.Intrusion-Related Gold Deposits.In:Sillitoe,R.H.,ed.,Gold Metallogeny and Exploration.Springer,Boston,MA,165-209.
Sillitoe,R.H.,2008.Major Gold Deposits and Belts of the North and South American Cordillera:Distribution,Tectonomagmatic Settings,and Metallogenic Considerations.Economic Geology,103(4):663-687.
Sillitoe,R.H.,Thompson,J.F.H.,1998.Intrusion-Related Vein Gold Deposits:Types,Tectono-Magmatic Settings and Difficulties of Distinction from Orogenic Gold Deposits.Resource Geology,48(4):237-250.https://doi.org/10.1111/j.1751-3928.1998.tb00021.x
Song,Y.,Jiang,S.H.,Bagas,L.,et al.,2016.The Geology and Geochemistry of Jinchangyu Gold Deposit,North China Craton:Implications for Metallogenesis and Geodynamic Setting.Ore Geology Reviews,73:313-329.https://doi.org/10.1016/j.oregeorev.2014.10.031
Spence-Jones,C.P.,Jenkin,G.R.T.,Boyce,A.J.,et al.,2018.Tellurium,Magmatic Fluids and Orogenic Gold:An Early Magmatic Fluid Pulse at Cononish Gold Deposit,Scotland.Ore Geology Reviews,102:894-905.https://doi.org/10.1016/j.oregeorev.2018.05.014
Standish,C.D.,Dhuime,B.,Chapman,R.J.,et al.,2014.The Genesis of Gold Mineralisation Hosted by Orogenic Belts:A Lead Isotope Investigation of Irish Gold Deposits.Chemical Geology,378-379:40-51.https://doi.org/10.1016/j.chemgeo.2014.04.012
Steadman,J.A.,Large,R.R.,2016.Synsedimentary,Diagenetic,and Metamorphic Pyrite,Pyrrhotite,and Marcasite at the Homestake BIF-Hosted Gold Deposit,South Dakota,USA:Insights on Au-As Ore Genesis from Textural and LA-ICP-MS Trace Element Studies.Economic Geology,111(7):1731-1752.https://doi.org/10.2113/econgeo.111.7.1731
Steadman,J.A.,Large,R.R.,Meffre,S.,et al.,2013.Age,Origin and Significance of Nodular Sulfides in 2 680 Ma Carbonaceous Black Shale of the Eastern Goldfields Superterrane,Yilgarn Craton,Western Australia.Precambrian Research,230:227-247.https://doi.org/10.1016/j.precamres.2013.02.013
Streit,J.E.,Cox,S.F.,2001.Fluid Pressures at Hypocenters of Moderate to Large Earthquakes.Journal of Geophysical Research:Solid Earth,106(B2):2235-2243.https://doi.org/10.1029/2000jb900359
Stüwe,K.,1998.Heat Sources of Cretaceous Metamorphism in the Eastern Alps:A Discussion.Tectonophysics,287(1-4):251-269.https://doi.org/10.1016/s0040-1951(98)80072-3
Sun,X.M.,Wei,H.X.,Zhai,W.,et al.,2014.Bangbu:The Largest Cenozic Orogenic Gold Deposit in Southern Tibet,China.Acta Geologica Sinica(English Edition),88(Suppl.2):788-789.
Sun,X.M.,Wei,H.X.,Zhai,W.,et al.,2016.Fluid Inclusion Geochemistry and Ar-Ar Geochronology of the Cenozoic Bangbu Orogenic Gold Deposit,Southern Tibet,China.Ore Geology Reviews,74:196-210.https://doi.org/10.1016/j.oregeorev.2015.11.021
Sun,X.M.,Zhang,Y.,Xiong,D.X.,et al.,2009.Crust and Mantle Contributions to Gold-Forming Process at the Daping Deposit,Ailaoshan Gold Belt,Yunnan,China.Ore Geology Reviews,36(1-3):235-249.https://doi.org/10.1016/j.oregeorev.2009.05.002
Tang,J.,Zheng,Y.F.,Wu,Y.B.,et al.,2007.Geochronology and Geochemistry of Metamorphic Rocks in the Jiaobei Terrane:Constraints on Its Tectonic Affinity in the Sulu Orogen.Precambrian Research,152(1-2):48-82.https://doi.org/10.1016/j.precamres.2006.09.001
Tang,L.,Santosh,M.,2018.Neoarchean Granite-Greenstone Belts and Related Ore Mineralization in the North China Craton:An Overview.Geoscience Frontiers,9(3):751-768.
Tomkins,A.G.,2010.Windows of Metamorphic Sulfur Liberation in the Crust:Implications for Gold Deposit Genesis.Geochimica et Cosmochimica Acta,74(11):3246-3259.https://doi.org/10.1016/j.gca.2010.03.003
Tomkins,A.G.,Grundy,C.,2009.Upper Temperature Limits of Orogenic Gold Deposit Formation:Constraints from the Granulite-Hosted Griffin's Find Deposit,Yilgarn Craton.Economic Geology,104(5):669-685.https://doi.org/10.2113/gsecongeo.104.5.669
Tripp,G.I.,Vearncombe,J.R.,2004.Fault/fracture Density and Mineralization:A Contouring Method for Targeting in Gold Exploration.Journal of Structural Geology,26(6-7):1087-1108.https://doi.org/10.1016/j.jsg.2003.11.002
Vearncombe,J.R.,1998.Shear Zones,Fault Networks,and Archean Gold.Geology,26(9):855.
Wall,V.J.,Graupner,T.,Yantsen,V.,et al.,2004.Muruntau,Uzbekistan:A Giant Thermal Aureole Gold(TAG)System.In:Muhling,J.,Goldfarb,R.,Vielreicher,N.,et al.,eds.,SEG 2004:Predictive Mineral Discovery Under Cover:Extended Abstracts:Centre for Global Metallogeny.University of Western Australia Publication,Perth,Australia,199-203.
Wang,C.S.,Liu,Z.F.,Hébert,R.,2000.The Yarlung-Zangbo Paleo-Ophiolite,Southern Tibet:Implications for the Dynamic Evolution of the Yarlung-Zangbo Suture Zone.Journal of Asian Earth Sciences,18(6):651-661.
Wang,Q.F.,Deng,J.,Groves,D.I.,Ore-Controlling Structure and Genesis of Orogenic Gold Deposit with Evolving Orogenesis:Case Study from Miocene Ailaoshan Orogenic Gold Deposits,TibetSoutheastern.Mineralium Deposita(in review).
Wang,Q.F.,Deng,J.,Liu,H.,et al.,2010a.Fractal Models for Ore Reserve Estimation.Ore Geology Reviews,37(1):2-14.https://doi.org/10.1016/j.oregeorev.2009.11.002
Wang,Q.F.,Deng,J.,Zhao,J.,et al.,2010b.Tonnage-Cutoff Model and Average Grade-Cutoff Model for a Single Ore Deposit.Ore Geology Reviews,38(1-2):113-120.https://doi.org/10.1016/j.oregeorev.2010.07.003
Wang,R.,Richards,J.P.,Zhou,L.M.,et al.,2015b.The Role of Indian and Tibetan Lithosphere in Spatial Distribution of Cenozoic Magmatism and Porphyry Cu-Mo Deposits in the Gangdese Belt,Southern Tibet.Earth-Science Reviews,150:68-94.
Wang,X.M.,Shao,S.C.,Wang,D.B.,2000.The Features and Geological Significance of Inclusion and Hydrogen and Oxygen Isotopes in Western Qinling Area.Journal of Precious Metallic Geology:9(1):44-48(in Chinese with English abstract).
Wang,Y.J.,Fan,W.M.,Zhang,G.W.,et al.,2013.Phanerozoic Tectonics of the South China Block:Key Observations and Controversies.Gondwana Research,23(4):1273-1305.https://doi.org/10.1016/j.gr.2012.02.019
Wang,Z.L.,Yang,L.Q.,Guo,L.N.,et al.,2015a.Fluid Immiscibility and Gold Deposition in the Xincheng Deposit,Jiaodong Peninsula,China:A Fluid Inclusion Study.Ore Geology Reviews,65:701-717.https://doi.org/10.1016/j.oregeorev.2014.06.006
Weatherley,D.K.,Henley,R.W.,2013.Flash Vaporization during Earthquakes Evidenced by Gold Deposits.Nature Geoscience,6(4):294-298.https://doi.org/10.1038/ngeo1759
Webber,A.P.,Roberts,S.,Taylor,R.N.,et al.,2013.Golden Plumes:Substantial Gold Enrichment of Oceanic Crust during Ridge-Plume Interaction.Geology,41(1):87-90.https://doi.org/10.1130/g33301.1
Weinberg,R.F.,Hodkiewicz,P.F.,Groves,D.I.,2004.What Controls Gold Distribution in Archean Terranes?Geology,32(7):545-548.https://doi.org/10.1130/g20475.1
Weller,O.M.,St-Onge,M.R.,Waters,D.J.,et al.,2013.Quantifying Barrovian Metamorphism in the Danba Structural Culmination of Eastern Tibet.Journal of Metamorphic Geology,31(9):909-935.https://doi.org/10.1111/jmg.12050
Whitney,D.L.,Teyssier,C.,Fayon,A.K.,2004.Isothermal Decompression,Partial Melting and Exhumation of Deep Continental Crust.Geological Society,London,Special Publications,227(1):313-326.https://doi.org/10.1144/gsl.sp.2004.227.01.16
Williams,H.M.,Turner,S.P.,Kelley,S.,et al.,2001.Age and Composition of Dikes in Southern Tibet:New Constraints on the Timing of East-West Extension and Its Relationship to Postcollisional Volcanism.Geology,29(4):339-342.
Williams,H.M.,Turner,S.P.,Pearce,J.A.,et al.,2004.Nature of the Source Regions for Post-Collisional,Potassic Magmatism in Southern and Northern Tibet from Geochemical Variations and Inverse Trace Element Modelling.Journal of Petrology,45(3):555-607.
Williams-Jones,A.E.,Bowell,R.J.,Migdisov,A.A.,2009.Gold in Solution.Elements,5(5):281-287.
Wintsch,R.P.,Christoffersen,R.,Kronenberg,A.K.,1995.Fluid-Rock Reaction Weakening of Fault Zones.Journal of Geophysical Research:Solid Earth,100(B7):13021-13032.https://doi.org/10.1029/94jb02622
Wyman,D.A.,1989.Archean Shoshonitic Lamprophyres Associated with Superior Province Gold Deposits:Distribution,Tectonic Setting,Noble Metal Abundances,and Significance for Gold Mineralization.Economic Geology Monographs,6:661-667.
Wyman,D.A.,Kerrich,R.,2010.Mantle Plume-Volcanic Arc Interaction:Consequences for Magmatism,Metallogeny,and Cratonization in the Abitibi and Wawa Subprovinces,Canada.Canadian Journal of Earth Sciences,47(5):565-589.https://doi.org/10.1139/e09-049
Wyman,D.A.,O’Neill,C.O.,Ayer,J.A.,2008.Evidence for Modern-Style Subduction to 3.1 Ga:A Plateau-AdakiteGold(Diamond)Association.The Geological Society of America,440:129-148.
Yang,J.H.,Wu,F.Y.,Wilde,S.A.,2003.A Review of the Geodynamic Setting of Large-Scale Late Mesozoic Gold Mineralization in the North China Craton:An Association with Lithospheric Thinning.Ore Geology Reviews,23(3-4):125-152.https://doi.org/10.1016/s0169-1368(03)00033-7
Yang,L.,Wang,Q.F.,Liu,X.F.,2015.Correlation between Mineralization Intensity and Fluid-Rock Reaction in the Xinli Gold Deposit,Jiaodong Peninsula,China:Constraints from Petrographic and Statistical Approaches.Ore Geology Reviews,71:29-39.https://doi.org/10.1016/j.oregeorev.2015.04.005
Yang,L.,Wang,Q.F.,Wang,Y.N.,et al.,2018b.Proto-to Paleo-Tethyan Evolution of the Eastern Margin of Simao Block.Gondwana Research,62:61-74.https://doi.org/10.1016/j.gr.2018.02.012
Yang,L.,Zhao,R.,Wang,Q.F.,et al.,2018a.Fault Geometry and Fluid-Rock Reaction:Combined Controls on Mineralization in the Xinli Gold Deposit,Jiaodong Peninsula,China.Journal of Structural Geology,111:14-26.https://doi.org/10.1016/j.jsg.2018.03.009
Yang,L.Q.,Deng,J.,Guo,C.Y.,et al.,2009a.Ore-Forming Fluid Characteristics of the Dayingezhuang Gold Deposit,Jiaodong Gold Province,China.Resource Geology,59(2):181-193.
Yang,L.Q.,Deng,J.,Guo,L.N.,et al.,2016a.Origin and Evolution of Ore Fluid,and Gold-Deposition Processes at the Giant Taishang Gold Deposit,Jiaodong Peninsula,Eastern China.Ore Geology Reviews,72:585-602.https://doi.org/10.1016/j.oregeorev.2015.08.021
Yang,L.Q.,Deng,J.,Wang,Z.L.,et al.,2016b.Thermochronologic Constraints on Evolution of the Linglong Metamorphic Core Complex and Implications for Gold Mineralization:A Case Study from the Xiadian Gold Deposit,Jiaodong Peninsula,Eastern China.Ore Geology Reviews,72:165-178.https://doi.org/10.1016/j.oregeorev.2015.07.006
Yang,L.Q.,Deng,J.,Wang,Z.L.,et al.,2016c.Relationships between Gold and Pyrite at the Xincheng Gold Deposit,Jiaodong Peninsula,China:Implications for Gold Source and Deposition in a Brittle Epizonal Environment.Economic Geology,111(1):105-126.https://doi.org/10.2113/econgeo.111.1.105
Yang,L.Y.,Yang,L.Q.,Yuan,W.M.,et al.,2013.Origin and Evolution of Ore Fluid for Orogenic Gold Traced by D-O Isotopes:A Case from the Jiapigou Gold Belt,China.Acta Petrologica Sinica,29(11):4025-4035.
Yang,Q.Y.,Santosh,M.,2015.Paleoproterozoic Arc Magmatism in the North China Craton:No Siderian Global Plate Tectonic Shutdown.Gondwana Research,28(1):82-105.
Yang,Z.S.,Hou,Z.Q.,Meng,X.J.,et al.,2009b.Post-Collisional Sb and Au Mineralization Related to the South Tibetan Detachment System,Himalayan Orogen.Ore Geology Reviews,36(1-3):194-212.
Yasuhara,H.,Polak,A.,Mitani,Y.,et al.,2006.Evolution of Fracture Permeability through Fluid-Rock Reaction under Hydrothermal Conditions.Earth and Planetary Science Letters,244(1-2):186-200.
Zhai,M.G.,Peng,P.,2007.Paleoproterozoic Events in the North China Craton.Acta Petrologica Sinica,23(11):2665-2682(in Chinese with English abstract).
Zhai,W.,Sun,X.M.,Yi,J.Z.,et al.,2014.Geology,Geochemistry,and Genesis of Orogenic Gold-Antimony Mineralization in the Himalayan Orogen,South Tibet,China.Ore Geology Reviews,58:68-90.https://doi.org/10.1016/j.oregeorev.2013.11.001
Zhai,Y.S.,Wang,J.P.,Peng,R.M.,et al.,2009.Research on Superimposed Metallogenic Systems and Polygenetic Mineral Deposits.Earth Science Frontiers,16(6):282-290(in Chinese with English abstract).
Zhang,G.Y.,Zheng,Y.Y.,Zhang,J.F.,et al.,2011.Ore-Control Structural and Geochronologic Constrain in Shalagang Antimony Deposit in Southern Tibet,China.Acta Petrologica Sinica,27(7):2143-2149(in Chinese with English abstract).
Zhang,H.F.,Parrish,R.,Zhang,L.,et al.,2007.A-Type Granite and Adakitic Magmatism Association in SongpanGarze Fold Belt,Eastern Tibetan Plateau:Implication for Lithospheric Delamination.Lithos,97(3-4):323-335.https://doi.org/10.1016/j.lithos.2007.01.002
Zhang,L.,Chen,H.Y.,Chen,Y.J.,et al.,2012.Geology and Fluid Evolution of the Wangfeng Orogenic-Type Gold Deposit,Western Tian Shan,China.Ore Geology Reviews,49:85-95.https://doi.org/10.1016/j.oregeorv.2012.09.002
Zhang,L.C.,Shen,Y.C.,Ji,J.S.,2003.Characteristics and Genesis of Kanggur Gold Deposit in the Eastern Tianshan Mountains,NW China:Evidence from Geology,Isotope Distribution and Chronology.Ore Geology Reviews,23(1-2):71-90.https://doi.org/10.1016/s0169-1368(03)00016-7
Zhang,L.C.,Zhou,X.H.,Ding,S.J.,2008.Mantle-Derived Fluids Involved in Large-Scale Gold Mineralization,Jiaodong District,China:Constraints Provided by the He-Ar and H-O Isotopic Systems.International Geology Review,50(5):472-482.https://doi.org/10.2747/0020-6814.50.5.472
Zhao,H.S.,Wang,Q.F.,Groves,D.I.,et al.,2019.A Rare Phanerozoic Amphibolite-Hosted Gold Deposit at Danba,Yangtze Craton,China:Significance to Fluid and Metal Sources for Orogenic Gold Systems.Mineralium Deposita,54(1):133-152.https://doi.org/10.1007/s00126-018-0845-x
Zhong,R.C.,Brugger,J.,Tomkins,A.G.,et al.,2015.Fate of Gold and Base Metals during Metamorphic Devolatilization of a Pelite.Geochimica et Cosmochimica Acta,171:338-352.doi:10.1016/j.gca.2015.09.013
Zhou,M.F.,Yan,D.P.,Kennedy,A.K.,et al.,2002a.SHRIMP U-Pb Zircon Geochronological and Geochemical Evidence for Neoproterozoic Arc-Magmatism along the Western Margin of the Yangtze Block,South China.Earth and Planetary Science Letters,196(1-2):51-67.https://doi.org/10.1016/s0012-821x(01)00595-7
Zhou,T.H.,Goldfarb,R.J.,Phillips,N.G.,2002b.Tectonics and Distribution of Gold Deposits in China:An Overview.Mineralium Deposita,37(3):249-282.
Zhou,M.F.,Yan,D.P.,Vasconcelos,P.M.,et al.,2008.Structural and Geochronological Constraints on the TectonoThermal Evolution of the Danba Domal Terrane,Eastern Margin of the Tibetan Plateau.Journal of Asian Earth Sciences,33(5-6):414-427.https://doi.org/10.1016/j.jseaes.2008.03.003
Zhu,L.H.,Qi,X.X.,Peng,S.B.,Li,Z.Q.,2011.Evolution of Ore Forming Fluid of Daping Gold Deposit in Ailaoshan Tectonic Zone,Southeast Tibet.Acta Petrologica Sinica,27(11):3395-3408.
Zhu,Y.N.,Peng,J.T.,2015.Infrared Microthermometric and Noble Gas Isotope Study of Fluid Inclusions in Ore Minerals at the Woxi Orogenic Au-Sb-W Deposit,Western Hunan,South China.Ore Geology Reviews,65:55-69.https://doi.org/10.1016/j.oregeorev.2014.08.014
毕献武,胡瑞忠,何明友,1997.哀牢山金矿带主要金矿床成矿流体特征.矿物学报,17(4):435-441.
陈衍景,Pirajno,F.,赖勇,等,2004.胶东矿集区大规模成矿时间和构造环境.岩石学报,20(4):907-922.
陈衍景,翟明国,蒋少涌,2009.华北大陆边缘造山过程与成矿研究的重要进展和问题.岩石学报,25(11):2695-2726.
邓军,杨立强,王长明,2011.三江特提斯复合造山与成矿作用研究进展.岩石学报,27(9):2501-2509.
李华健,王庆飞,杨林,等,2017.青藏高原碰撞造山背景造山型金矿床:构造背景、地质及地球化学特征.岩石学报,33(7):2189-2201.
李士辉,张静,邓军,等,2011.哀牢山南段长安金矿床成矿流体特征及成因类型探讨.岩石学报,27(12):3777-3786.
梁业恒,孙晓明,石贵勇,等,2011.云南哀牢山老王寨大型造山型金矿成矿流体地球化学.岩石学报,27(9):2533-2540.
毛景文,谢桂青,李晓峰,等,2004.华南地区中生代大规模成矿作用与岩石圈多阶段伸展.地学前缘,11(1):45-55.
毛景文,谢桂青,张作衡,等,2005.中国北方中生代大规模成矿作用的期次及其地球动力学背景.岩石学报,21(1):169-188.
王学明,邵世才,汪东波,等,2000.西秦岭金矿床包裹体、氢氧同位素特征及其地质意义.贵金属地质,9(1):44-48.
翟明国,彭澎,2007.华北克拉通古元古代构造事件.岩石学报,23(11):2665-2682.
翟裕生,王建平,彭润民,等,2009.叠加成矿系统与多成因矿床研究.地学前缘,16(6):282-290.
张刚阳,郑有业,张建芳,等,2011.西藏沙拉岗锑矿控矿构造及成矿时代约束.岩石学报,27(7):2143-2149.
Barley,M.E.,Groves,D.I.,1992.Supercontinent Cycles and the Distribution of Metal Deposits through Time.Geology,20(4):291-294.
Bath,A.B.,Walshe,J.L.,Cloutier,J.,et al.,2013.Biotite and Apatite as Tools for Tracking Pathways of Oxidized Fluids in the Archean East Repulse Gold Deposit,Australia.Economic Geology,108(4):667-690.https://doi.org/10.2113/econgeo.108.4.667
Bell,R.M.,Kolb,J.,Waight,T.E.,2018.Assessment of Lithological,Geochemical and Structural Controls on Gold Distribution in the Nalunaq Gold Deposit,South Greenland Using Three-Dimensional Implicit Modelling.Geological Society,London,Special Publications,453(1):385-405.https://doi.org/10.1144/sp453.2
Bi,X.W.,Hu,R.Z.,He,M.Y.,1997.Characteristics of OreForming Fluid of Three Gold Deposits in Ailaoshan Gold Mineralization Belt.Acta Mineralogica Sinica,17(4):435-441(in Chinese with English abstract).
Bierlein,F.P.,Crowe,D.E.,2000.Phanerozoic Orogenic Lode Gold Deposits.Reviews in Economic Geology,13:103-139.
Bierlein,F.P.,Groves,D.I.,Goldfarb,R.J.,et al.,2006.Lithospheric Controls on the Formation of Provinces Hosting Giant Orogenic Gold Deposits.Mineralium Deposita,40(8):874-886.https://doi.org/10.1007/s00126-005-0046-2
Bierlein,F.P.,Maher,S.,2001.Orogenic Disseminated Gold in Phanerozoic Fold Belts:Examples from Victoria,Australia and Elsewhere.Ore Geology Reviews,18(1-2):113-148.https://doi.org/10.1016/s0169-1368(01)00019-1
Bierlein,F.P.,Pisarevsky,S.,2008.Plume-Related Oceanic Plateaus as a Potential Source of Gold Mineralization.Economic Geology,103(2):425-430.https://doi.org/10.2113/gsecongeo.103.2.425
Blenkinsop,T.G.,Doyle,M.G.,2014.Structural Controls on Gold Mineralization on the Margin of the Yilgarn Craton,Albany-Fraser Orogen:The Tropicana Deposit,Western Australia.Journal of Structural Geology,67:189-204.https://doi.org/10.1016/j.jsg.2014.01.013
Bouchot,V.,Ledru,P.,Lerouge,C.,et al.,2005.Late Variscan Mineralizing Systems Related to Orogenic Processes:The French Massif Central.Ore Geology Reviews,27(1-4):169-197.https://doi.org/10.1016/j.oregeorev.2005.07.017
Breeding,C.M.,Ague,J.J.,2002.Slab-Derived Fluids and Quartz-Vein Formation in an Accretionary Prism,Otago Schist,New Zealand.Geology,30(6):499-502.
Browning,P.,Groves,D.I.,Blockley,J.G.,et al.,1987.Lead Isotope Constraints on the Age and Source of Gold Mineralization in the Archean Yilgarn Block,Western Australia.Economic Geology,82(4):971-986.https://doi.org/10.2113/gsecongeo.82.4.971
Bucher,K.,Grapes,R.,2011.Metamorphism of Pelitic Rocks(Metapelites).Petrogenesis of Metamorphic Rocks.Springer,Heidelberg,Berlin,257-313.
Bureau,H.,Keppler,H.,1999.Complete Miscibility between Silicate Melts and Hydrous Fluids in the Upper Mantle:Experimental Evidence and Geochemical Implications.Earth and Planetary Science Letters,165(2):187-196.https://doi.org/10.1016/s0012-821x(98)00266-0
Burnard,P.G.,Polya,D.A.,2004.Importance of Mantle Derived Fluids during Granite Associated Hydrothermal Circulation:He and Ar Isotopes of Ore Minerals from Panasqueira.Geochimica et Cosmochimica Acta,68(7):1607-1615.https://doi.org/10.1016/j.gca.2003.10.008
Cao,S.Y.,Liu,J.L.,Leiss,B.,et al.,2011.Oligo-Miocene Shearing along the Ailao Shan-Red River Shear Zone:Constraints from Structural Analysis and Zircon U/Pb Geochronology of Magmatic Rocks in the Diancang Shan Massif,SE Tibet,China.Gondwana Research,19(4):975-993.https://doi.org/10.1016/j.gr.2010.10.006
Carrier,A.,Jebrak,M.,Angelier,J.,et al.,2000.The Silidor Deposit,Rouyn-Noranda District,Abitibi Belt:Geology,Structural Evolution,and Paleostress Modeling of an Au Quartz Vein-Type Deposit in an Archean Trondhjemite.Economic Geology,95(5):1049-1065.
Chen,M.H.,Mao,J.W.,Bierlein,F.P.,et al.,2011.Structural Features and Metallogenesis of the Carlin-Type Jinfeng(Lannigou)Gold Deposit,Guizhou Province,China.Ore Geology Reviews,43(1):217-234.https://doi.org/10.1016/j.oregeorev.2011.06.009
Chen,Y.J.,Pirajno,F.,Lai,Y.,et al.,2004.Metallogenic Time and Tectonic Setting of the Jiaodong Gold Province,Eastern China.Acta Petrologica Sinica,20(4):907-922(in Chinese with English abstract).
Chen,Y.J.,Pirajno,F.,Qi,J.P.,2008.The Shanggong Gold Deposit,Eastern Qinling Orogen,China:Isotope Geochemistry and Implications for Ore Genesis.Journal of Asian Earth Sciences,33(3-4):252-266.https://doi.org/10.1016/j.jseaes.2007.12.002
Chen,Y.J.,Zhai,M.G.,Jiang,S.Y.,2009.Significant Achievements and Open Issues in Study of Orogenesis and Metallogenesis Surrounding the North China Continent.Acta Petrologica Sinica,25(11):2695-2726(in Chinese with English abstract).
Christie,A.B.,Brathwaite,R.L.,2003.Hydrothermal Alteration in Metasedimentary Rock-Hosted Orogenic Gold Deposits,Reefton Goldfield,South Island,New Zealand.Mineralium Deposita,38(1):87-107.https://doi.org/10.1007/s00126-002-0280-9
Connolly,J.A.D.,Cesare,B.,1993.C-O-H-S Fluid Composition and Oxygen Fugacity in Graphitic Metapelites.Journal of Metamorphic Geology,11(3):379-388.https://doi.org/10.1111/j.1525-1314.1993.tb00155.x
Cox,S.F.,2010.The Application of Failure Mode Diagrams for Exploring the Roles of Fluid Pressure and Stress States in Controlling Styles of Fracture-Controlled Permeability Enhancement in Faults and Shear Zones.Geofluids,10:217-233.https://doi.org/10.1111/j.1468-8123.2010.00281.x
Cox,S.F.,2016.Injection-Driven Swarm Seismicity and Permeability Enhancement:Implications for the Dynamics of Hydrothermal Ore Systems in High Fluid-Flux,OverpressuredFaulting Regimes:An Invited Paper.Economic Geology,111(3):559-587.https://doi.org/10.2113/econgeo.111.3.559
Cox,S.F.,2019.The Dynamics of Permeability Enhancement and Fluid Flow in Overpressured,Fracture Controlled Hydrothermal Systems.Economic Geology(in press).
Cox,S.F.,Etheridge,M.A.,Cas,R.A.F.,et al.,1991.Deformational Style of the Castlemaine Area,Bendigo-Ballarat Zone:Implications fore Volution of Crustal Structure in Central Victoria.Australian Journal of Earth Sciences,38(2):151-170.
Dai,J.G.,Wang,C.S.,Li,Y.L.,2012.Relicts of the Early Cretaceous Seamounts in the Central-Western Yarlung Zangbo Suture Zone,Southern Tibet.Journal of Asian Earth Sciences,53:25-37.https://doi.org/10.1016/j.jseaes.2011.12.024
Davis,G.A.,Darby,B.J.,Zheng,Y.D.,et al.,2002.Geometric and Temporal Evolution of an Extensional Detachment Fault,Hohhot Metamorphic Core Complex,Inner Mongolia,China.Geology,30(11):1003-1006.
De Boorder,H.,2012.Spatial and Temporal Distribution of the Orogenic Gold Deposits in the Late Palaeozoic Variscides and Southern Tianshan:How Orogenic are They?Ore Geology Reviews,46:1-31.https://doi.org/10.1016/j.oregeorev.2012.01.002
Deng,J.,Liu,X.F.,Wang,Q.F.,et al.,2015a.Origin of the Jiaodong-Type Xinli Gold Deposit,Jiaodong Peninsula,China:Constraints from Fluid Inclusion and C-D-O-S-Sr Isotope Compositions.Ore Geology Reviews,65:674-686.https://doi.org/10.1016/j.oregeorev.2014.04.018
Deng,J.,Wang,Q.F.,Li,G.J.,et al.,2015b.Structural Control and Genesis of the Oligocene Zhenyuan Orogenic Gold Deposit,SW China.Ore Geology Reviews,65:42-54.https://doi.org/10.1016/j.oregeorev.2014.08.002
Deng,J.,Wang,C.M.,Bagas,L.,et al.,2015c.Cretaceous-Cenozoic Tectonic History of the Jiaojia Fault and Gold Mineralization in the Jiaodong Peninsula,China:Constraints from Zircon U-Pb,Illite K-Ar,and Apatite Fission Track Thermochronometry.Mineralium Deposita,50(8):987-1006.https://doi.org/10.1007/s00126-015-0584-1
Deng,J.,Wang,Q.F.,2016.Gold Mineralization in China:Metallogenic Provinces,Deposit Types and Tectonic Framework.Gondwana Research,36:219-274.https://doi.org/10.1016/j.gr.2015.10.003
Deng,J.,Wang,Q.F.,Li,G.J.,et al.,2014a.Tethys Tectonic Evolution and Its Bearing on the Distribution of Important Mineral Deposits in the Sanjiang Region,SW China.Gondwana Research,26(2):419-437.https://doi.org/10.1016/j.gr.2013.08.002
Deng,J.,Wang,Q.F.,Li,G.J.,et al.,2014b.CenozoicTectono-Magmatic and Metallogenic Processes in the Sanjiang Region,Southwestern China.Earth-Science Reviews,138:268-299.https://doi.org/10.1016/j.earscirev.2014.05.015
Deng,J.,Yuan,W.M.,Carranza,E.J.M.,et al.,2014c.Geochronology and Thermochronometry of the Jiapigou Gold Belt,Northeastern China:New Evidence for Multiple Episodes of Mineralization.Journal of Asian Earth Sciences,89:10-27.
Deng,J.,Wang,Q.F.,Wan,L.,et al.,2009a.Self-Similar Fractal Analysis of Gold Mineralization of Dayingezhuang Disseminated-Veinlet Deposit in Jiaodong Gold Province,China.Journal of Geochemical Exploration,102(2):95-102.
Deng,J.,Yang,L.Q.,Gao,B.F.,et al.,2009b.Fluid Evolution and Metallogenic Dynamics during Tectonic Regime Transition:Example from the Jiapigou Gold Belt in Northeast China.Resource Geology,59(2):140-152.https://doi.org/10.1111/j.1751-3928.2009.00086.x
Deng,J.,Wang,Q.F.,Wan,L.,et al.,2011.A Multifractal Analysis of Mineralization Characteristics of the Dayingezhuang Disseminated-Veinlet Gold Deposit in the Jiaodong Gold Province of China.Ore Geology Reviews,40(1):54-64.
Deng,J.,Wang,Q.F.,Yang,L.Q.,et al.,2010a.Delineation and Explanation of Geochemical Anomalies Using Fractal Models in the Heqing Area,Yunnan Province,China.Journal of Geochemical Exploration,105(3):95-105.https://doi.org/10.1016/j.gexplo.2010.04.005
Deng,J.,Yang,L.Q.,Sun,Z.S.,et al.,2010b.A Metallogenic Model of Gold Deposits of the Jiaodong Granite-Greenstone Belt.Acta Geologica Sinica(English Edition),77(4):537-546.
Deng,J.,Yang,L.Q.,Wang,C.M.,2011.Research Advances of Superimposed Orogenesis and Metallogenesis in the Sanjiang Tethys.Acta Petrologica Sinica,27(9):2501-2509(in Chinese with English abstract).
Ding,Q.F.,Jiang,S.Y.,Sun,F.Y.,2014.Zircon U-Pb Geochronology,Geochemical and Sr-Nd-Hf Isotopic Compositions of the Triassic Granite and Diorite Dikes from the Wulonggou Mining Area in the Eastern Kunlun Orogen,NW China:Petrogenesis and Tectonic Implications.Lithos,205:266-283.https://doi.org/10.1016/j.lithos.2014.07.015
Drummond,B.J.,Goleby,B.R.,Swager,C.P.,et al.,1993.Constraints on Archean Crustal Composition and Structure Provided by Deep Seismic Sounding in the Yilgarn Block.Ore Geology Reviews,8(1-2):117-124.
Du,J.X.,Zhang,L.F.,Bader,T.,et al.,2014.Metamorphic Evolution of Ultrahigh-Pressure Rocks from Chinese Southwestern Tianshan and a Possible Indicator of UHP-Metamorphism Using Garnet Composition in Low-TEclogites.Journal of Asian Earth Sciences,91:69-88.https://doi.org/10.1016/j.jseaes.2014.04.010
Dziggel,A.,Poujol,M.,Otto,A.,et al.,2010.New U-Pb and40Ar/39Ar Ages from the Northern Margin of the Barberton Greenstone Belt,South Africa:Implications for the Formation of Mesoarchaean Gold Deposits.Precambrian Research,179(1-4):206-220.https://doi.org/10.1016/j.precamres.2010.03.006
Eisenlohr,B.N.,Groves,D.I.,Partington,G.A.,1989.CrustalScale Shear Zones and Their Significance to Archaean Gold Mineralization in Western Australia.Mineralium Deposita,24(1):1-8.
Elmer,F.L.,White,R.W.,Powell,R.,2006.Devolatilization of Metabasic Rocks during Greenschist-Amphibolite Facies Metamorphism.Journal of Metamorphic Geology,24(6):497-513.https://doi.org/10.1111/j.1525-1314.2006.00650.x
Evans,K.A.,2010.A Test of the Viability of Fluid-Wall Rock Interaction Mechanisms for Changes in Opaque Phase Assemblage in Metasedimentary Rocks in the Kambalda-St.Ives Goldfield,Western Australia.Mineralium Deposita,45(2):207-213.
Evans,K.A.,Phillips,G.N.,Powell,R.,2006.Rock-Buffering of Auriferous Fluids in Altered Rocks Associated with the Golden Mile-Style Mineralization,Kalgoorlie Gold Field,Western Australia.Economic Geology,101(4):805-817.https://doi.org/10.2113/gsecongeo.101.4.805
Fan,H.R.,Zhai,M.G.,Xie,Y.H.,et al.,2003.Ore-Forming Fluids Associated with Granite-Hosted Gold Mineralization at the Sanshandao Deposit,Jiaodong Gold Province,China.Mineralium Deposita,38(6):739-750.https://doi.org/10.1007/s00126-003-0368-x
Finch,E.G.,Tomkins,A.G.,2017.Pyrite-Pyrrhotite Stability in a Metamorphic Aureole:Implications for Orogenic Gold Genesis.Economic Geology,112(3):661-674.https://doi.org/10.2113/econgeo.112.3.661
Finlay,A.J.,Selby,D.,Osborne,M.J.,et al.,2010.FaultCharged Mantle-Fluid Contamination of United Kingdom North Sea Oils:Insights from Re-Os Isotopes.Geology,38(11):979-982.https://doi.org/10.1130/g31201.1
Fridovsky,V.Y.,2017.Structural Control of Orogenic Gold Deposits of the Verkhoyansk-Kolyma Folded Region,Northeast Russia.Ore Geology Reviews,103:38-55.https://doi.org/10.1016/j.oregeorev.2017.01.006
Fu,B.,Touret,J.L.R.,2014.From Granulite Fluids to QuartzCarbonate Megashear Zones:The Gold Rush.Geoscience Frontiers,5(5):747-758.https://doi.org/10.1016/j.gsf.2014.03.013
Gao,L.,Wang,Q.F.,Deng,J.,et al.,2018.Relationship between Orogenic Gold Mineralization and Crustal Shearing along Ailaoshan-Red River Belt,Southeastern Tibetan Plateau:New Constraint from Paleomagnetism.Geochemistry,Geophysics,Geosystems,19(7):2225-2242.https://doi.org/10.1029/2018gc007493
Gebre-Mariam,M.,Hagemann,S.G.,Groves,D.I.,1995.AClassification Scheme for Epigenetic Archaean LodeGold Deposits.Mineralium Deposita,30(5):408-410.
Goldfarb,R.J.,Baker,T.,Dube,B.,et al.,2005.Distribution,Character,and Genesis of Gold Deposits in Metamorphic Belts.In:Hedenquist,J.W.,Thompson,J.F.H.,Goldfarb,J.,eds.,Economic Geology 100th Anniversary Volume.Society of Economic Geologists,Littleton,Colorado,USA,407-450.
Goldfarb,R.J.,Groves,D.I.,2015.Orogenic Gold:Common or Evolving Fluid and Metal Sources through Time.Lithos,233:2-26.https://doi.org/10.1016/j.lithos.2015.07.011
Goldfarb,R.J.,Groves,D.I.,Gardoll,S.,2001.Orogenic Gold and Geologic Time:A Global Synthesis.Ore Geology Reviews,18(1-2):1-75.https://doi.org/10.1016/s0169-1368(01)00016-6
Goldfarb,R.J.,Hart,C.,Davis,G.,et al.,2007.East Asian Gold:Deciphering the Anomaly of Phanerozoic Gold in Precambrian Cratons.Economic Geology,102(3):341-345.https://doi.org/10.2113/gsecongeo.102.3.341
Goldfarb,R.J.,Santosh,M.,2014.The Dilemma of the Jiaodong Gold Deposits:Are They Unique?Geoscience Frontiers,5(2):139-153.https://doi.org/10.1016/j.gsf.2013.11.001
Griffin,W.L.,Begg,G.C.,O'Reilly,S.Y.,2013.ContinentalRoot Control on the Genesis of Magmatic Ore Deposits.Nature Geoscience,6(11):905-910.https://doi.org/10.1038/ngeo1954
Groves,D.,Barnicoat,A.C.,Barley,M.,et al.,1992.SubGreenschist to Granulite-Hosted Archaean Lode-Gold Deposits of the Yilgarn Craton:A Depositional Continuum from Deep-Sourced Hydrothermal Fluids in Crustalscale Plumbing Systems.Geology Department(Key Centre)and University Extension.The University of Western Australia Publication,Perth,Australia,325-338.
Groves,D.I.,1993.The Crustal Continuum Model for LateArchaean Lode-Gold Deposits of the Yilgarn Block,Western Australia.Mineralium Deposita,28(6):366-374.
Groves,D.I.,Condie,K.C.,Goldfarb,R.J.,et al.,2005.100th Anniversary Special Paper:Secular Changes in Global Tectonic Processes and Their Influence on the Temporal Distribution of Gold-Bearing Mineral Deposits.Economic Geology,100(2):203-224.https://doi.org/10.2113/gsecongeo.100.2.203
Groves,D.I.,Goldfarb,R.J.,Gebre-Mariam,M.,et al.,1998.Orogenic Gold Deposits:A Proposed Classification in the Context of Their Crustal Distribution and Relationship to Other Gold Deposit Types.Ore Geology Reviews,13(1-5):7-27.https://doi.org/10.1016/s0169-1368(97)00012-7
Groves,D.I.,Goldfarb,R.J.,Robert,F.,et al.,2003.Gold Deposits in Metamorphic Belts:Overview of Current Understanding,Outstanding Problems,Future Research,and Exploration Significance.Economic Geology,98(1):1-29.https://doi.org/10.2113/gsecongeo.98.1.1
Groves,D.I.,Santosh,M.,2015.Province-Scale Commonalities of Some World-Class Gold Deposits:Implications for Mineral Exploration.Geoscience Frontiers,6(3):389-399.https://doi.org/10.1016/j.gsf.2014.12.007
Groves,D.I.,Santosh,M.,2016.The Giant Jiaodong Gold Province:The Key to a Unified Model for Orogenic Gold Deposits?Geoscience Frontiers,7(3):409-417.
Groves,D.I.,Santosh,M.,Deng,J.,et al.,2019.A Holistic Model for the Origin of Orogenic Gold Deposits and Its Implications for Exploration.Mineralium Deposita.https://doi.org/10.1007/s00126-019-0087-5.
Groves,D.I.,Santosh,M.,Goldfarb,R.J.,et al.,2018.Structural Geometry of Orogenic Gold Deposits:Implications for Exploration of World-Class and Giant Deposits.Geoscience Frontiers,9(4):1163-1177.
Gumiel,P.,Sanderson,D.J.,Arias,M.,et al.,2010.Analysis of the Fractal Clustering of Ore Deposits in the Spanish Iberian Pyrite Belt.Ore Geology Reviews,38(4):307-318.https://doi.org/10.1016/j.oregeorev.2010.08.001
Guo,Z.F.,Wilson,M.,Zhang,M.L.,et al.,2013.Post-Collisional,K-Rich Mafic Magmatism in South Tibet:Constraints on Indian Slab-to-Wedge Transport Processes and Plateau Uplift.Contributions to Mineralogy and Petrology,165(6):1311-1340.https://doi.org/10.1007/s00410-013-0860-y
Haddad-Martim,P.M.,Carranza,E.J.M.,de Souza Filho,C.R.,2018.The Fractal Nature of Structural Controls on Ore Formation:The Case of the Iron Oxide Copper-Gold Deposits in the Carajás Mineral Province,Brazilian Amazon.Economic Geology,113(7):1499-1524.https://doi.org/10.5382/econgeo.2018.4600
Harrison,T.M.,Yin,A.,Grove,M.,et al.,2000.The Zedong Window:A Record of Superposed Tertiary Convergence in Southeastern Tibet.Journal of Geophysical Research:Solid Earth,105(B8):19211-19230.https://doi.org/10.1029/2000jb900078
Hart,C.,2005.Classifying,Distinguishing and Exploring for Intrusion-Related Gold Systems.The Gangue,87(1):9.
Helt,K.M.,Williams-Jones,A.E.,Clark,J.R.,et al.,2014.Constraints on the Genesis of the Archean Oxidized,Intrusion-Related Canadian Malartic Gold Deposit,Quebec,Canada.Economic Geology,109(3):713-735.https://doi.org/10.2113/econgeo.109.3.713
Hodkiewicz,P.F.,Groves,D.I.,Davidson,G.J.,et al.,2009.Influence of Structural Setting on Sulphur Isotopes in Archean Orogenic Gold Deposits,Eastern Goldfields Province,Yilgarn,Western Australia.Mineralium Deposita,44(2):129-150.https://doi.org/10.1007/s00126-008-0211-5
Hou,Z.Q.,Cook,N.J.,2009.Metallogenesis of the Tibetan Collisional Orogen:A Review and Introduction to the Special Issue.Ore Geology Reviews,36(1-3):2-24.https://doi.org/10.1016/j.oregeorev.2009.05.001
Hou,Z.Q.,Duan,L.F.,Lu,Y.J.,et al.,2015.Lithospheric Architecture of the Lhasa Terrane and Its Control on Ore Deposits in the Himalayan-Tibetan Orogen.Economic Geology,110(6):1541-1575.https://doi.org/10.2113/econgeo.110.6.1541
Hou,Z.Q.,Zaw,K.,Pan,G.T.,et al.,2007.Sanjiang Tethyan Metallogenesis in S.W.China:Tectonic Setting,Metallogenic Epochs and Deposit Types.Ore Geology Reviews,31(1-4):48-87.https://doi.org/10.1016/j.oregeorv.2004.12.007
Hronsky,J.M.A.,Groves,D.I.,Loucks,R.R.,et al.,2012.AUnified Model for Gold Mineralisation in Accretionary Orogens and Implications for Regional-Scale Exploration Targeting Methods.Mineralium Deposita,47(4):339-358.https://doi.org/10.1007/s00126-012-0402-y
Hyndman,R.D.,McCrory,P.A.,Wech,A.,et al.,2015.Cascadia Subducting Plate Fluids Channelled to Fore-ArcMantle Corner:ETS and Silica Deposition.Journal of Geophysical Research:Solid Earth,120(6):4344-4358.https://doi.org/10.1002/2015jb011920
Jia,S.S.,Wang,E.D.,Fu,J.F.,et al.,2018.Indosinian Gold Mineralization and Magmatic-Hydrothermal Evolution of the Hadamengou Gold Deposit at the Northern Margin of the North China Craton:Constraints from K-Feldspar Laser40Ar/39Ar Dating.Journal of Geochemical Exploration,190:314-324.https://doi.org/10.1016/j.gexplo.2018.04.002
Jiang,S.H.,Nie,F.J.,Hu,P.,et al.,2009.Mayum:An Orogenic Gold Deposit in Tibet,China.Ore Geology Reviews,36(1-3):160-173.https://doi.org/10.1016/j.oregeorev.2009.03.006
Katayama,I.,Terada,T.,Okazaki,K.,et al.,2012.Episodic Tremor and Slow Slip Potentially Linked to Permeability Contrasts at the Moho.Nature Geoscience,5(10):731-734.https://doi.org/10.1038/ngeo1559
Kawano,S.,Katayama,I.,Okazaki,K.,2011.Permeability Anisotropy of Serpentinite and Fluid Pathways in a Subduction Zone.Geology,39(10):939-942.https://doi.org/10.1130/g32173.1
Kennedy,B.M.,1997.Mantle Fluids in the San Andreas Fault System,California.Science,278(5341):1278-1281.
Kennedy,B.M.,van Soest,M.C.,2007.Flow of Mantle Fluids through the Ductile Lower Crust:Helium Isotope Trends.Science,318(5855):1433-1436.
Kerrich,R.,Fyfe,W.S.,1981.The Gold:Carbonate Association,Source of CO2,and CO2Fixation Reactions in Archaean Lode Deposits.Chemical Geology,33(1-4):265-294.
Kerrich,R.,Goldfarb,R.,Groves,D.,et al.,2000.The Characteristics,Origins,and Geodynamic Settings of Supergiant Gold Metallogenic Provinces.Science in China(Series D),43(Suppl.1):1-68.
Kerrich,R.,Wyman,D.,1990.Geodynamic Setting of Mesothermal Gold Deposits:An Association with Accretionary Tectonic Regimes.Geology,18(9):882-825.
Klein-Ben David,O.,Pettke,T.,Kessel,R.,2011.Chromium Mobility in Hydrous Fluids at Upper Mantle Conditions.Lithos,125(1-2):122-130.
Klemperer,S.L.,Kennedy,B.M.,Sastry,S.R.,et al.,2013.Mantle Fluids in the Karakoram Fault:Helium Isotope Evidence.Earth and Planetary Science Letters,366:59-70.https://doi.org/10.1016/j.epsl.2013.01.013
Knight,J.T.,Groves,D.I.,Ridley,J.R.,1993.The Coolgardie Goldfied,Western Australia:District-Scale Controls on an Archaean Gold Camp in an Amphibolite Facies Terrane.Mineralium Deposita,28(6):436-456.
Knight,J.T.,Ridley,J.R.,Groves,D.I.,2000.The Archean Amphibolite Facies Coolgardie Goldfield,Yilgarn Craton,Western Australia:Nature,Controls,and Gold FieldScale Patterns of Hydrothermal Wall-Rock Alteration.Economic Geology,95(1):49-84.https://doi.org/10.2113/gsecongeo.95.1.49
Kolb,J.,Dziggel,A.,Bagas,L.,2015.Hypozonal Lode Gold Deposits:A Genetic Concept Based on a Review of the New Consort,Renco,Hutti,Hira Buddini,Navachab,Nevoria and the Granites Deposits.Precambrian Research,262:20-44.https://doi.org/10.1016/j.precamres.2015.02.022
Kolb,J.,Kisters,A.F.M.,Hoernes,S.,et al.,2000.The Origin of Fluids and Nature of Fluid-Rock Interaction in MidCrustal Auriferous Mylonites of the Renco Mine,Southern Zimbabwe.Mineralium Deposita,35(2-3):109-125.https://doi.org/10.1007/s001260050010
Kolb,J.,Meyer,M.F.,2002.Fluid Inclusion Record of the Hypozonal Orogenic Renco Gold Deposit(Zimbabwe)during the Retrograde P-T Evolution.Contributions to Mineralogy and Petrology,143(4):495-509.https://doi.org/10.1007/s00410-002-0360-y
Kolb,J.,Rogers,A.,Meyer,F.M.,2005.Relative Timing of Deformation and Two-Stage Gold Mineralization at the Hutti Mine,Dharwar Craton,India.Mineralium Deposita,40(2):156-174.
Kontak,D.J.,Smith,P.K.,Kerrich,R.,et al.,1990.Integrated Model for Meguma Group Lode Gold Deposits,Nova Scotia,Canada.Geology,18(3):238-242.
LaFlamme,C.,Jamieson,J.W.,Fiorentini,M.L.,et al.,2018.Investigating Sulfur Pathways through the Lithosphere by Tracing Mass Independent Fractionation of Sulfur to the Lady Bountiful Orogenic Gold Deposit,Yilgarn Craton.Gondwana Research,58:27-38.https://doi.org/10.1016/j.gr.2018.02.005
Large,R.R.,Bull,S.W.,Maslennikov,V.V.,2011.A Carbonaceous Sedimentary Source-Rock Model for CarlinType and Orogenic Gold Deposits.Economic Geology,106(3):331-358.https://doi.org/10.2113/econgeo.106.3.331
Large,R.R.,Danyushevsky,L.,Hollit,C.,et al.,2009.Gold and Trace Element Zonation in Pyrite Using a Laser Imaging Technique:Implications for the Timing of Gold in Orogenic and Carlin-Style Sediment-Hosted Deposits.Economic Geology,104(5):635-668.https://doi.org/10.2113/gsecongeo.104.5.635
Large,R.R.,Maslennikov,V.V.,Robert,F.,et al.,2007.Multistage Sedimentary and Metamorphic Origin of Pyrite and Gold in the Giant Sukhoi Log Deposit,Lena Gold Province,Russia.Economic Geology,102(7):1233-1267.https://doi.org/10.2113/gsecongeo.102.7.1233
Lawrence,D.M.,Treloar,P.J.,Rankin,A.H.,et al.,2013.The Geology and Mineralogy of the Loulo Mining District,Mali,West Africa:Evidence for Two Distinct Styles of Orogenic Gold Mineralization.Economic Geology,108(2):199-227.https://doi.org/10.2113/econgeo.108.2.199
Lebrun,E.,Miller,J.,Thébaud,N.,et al.,2017.Structural Controls on an Orogenic Gold System:The World-Class Siguiri Gold District,Siguiri Basin,Guinea,West Africa.Economic Geology,112(1):73-98.https://doi.org/10.2113/econgeo.112.1.73
Li,H.J.,Wang,Q.F.,Deng,J.,et al.,2019a.Alteration and Mineralization Styles of the Orogenic Disseminated Zhenyuan Gold Deposit,Southeastern Tibet:Contrast with Carlin Gold Deposit.Geoscience Frontiers.https://doi.org/10.1016/j.gsf.2019.01.008
Li,H.J.,Wang,Q.F.,Groves,D.I.,et al.,2019b.Alteration of Eocene Lamprophyres in the Zhenyuan Orogenic Gold Deposit,Yunnan Province,China:Composition and Evolution of Ore Fluids.Ore Geology Reviews,107:1068-1083.https://doi.org/10.1016/j.oregeorev.2019.03.032
Li,H.J.,Wang,Q.F.,Yang,L.,et al.,2017.Orogenic Gold Deposits Formed in Tibetan Collisional Orogen Setting:Geotectonic Setting,Geological and Geochemical Features.Acta Petrologica Sinica,33(7):2189-2201(in Chinese with English abstract).
Li,J.F.,Xia,B.,Liu,L.W.,et al.,2009.SHRIMP U-Pb Dating for the Gabbro in Qunrang Ophiolite,Tibet:The Geochronology Constraint for the Development of Eastern Tethys Basin.Geotectonica et Metallogenia,33(2):294-298.
Li,J.W.,Bi,S.J.,Selby,D.,et al.,2012a.Giant Mesozoic Gold Provinces Related to the Destruction of the North China Craton.Earth and Planetary Science Letters,349-350:26-37.https://doi.org/10.1016/j.epsl.2012.06.058
Li,J.W.,Li,Z.K.,Zhou,M.F.,et al.,2012b.The Early Cretaceous Yangzhaiyu Lode Gold Deposit,North China Craton:A Link between Craton Reactivation and Gold Veining.Economic Geology,107(1):43-79.
Li,J.W.,Vasconcelos,P.M.,Zhou,M.F.,et al.,2006.Geochronology of the Pengjiakuang and Rushan Gold Deposits,Eastern Jiaodong Gold Province,Northeastern China:Implications for Regional Mineralization and Geodynamic Setting.Economic Geology,101(5):1023-1038.https://doi.org/10.2113/gsecongeo.101.5.1023
Li,L.,Santosh,M.,Li,S.R.,2015.The‘Jiaodong Type’Gold Deposits:Characteristics,Origin and Prospecting.Ore Geology Reviews,65:589-611.https://doi.org/10.1016/j.oregeorev.2014.06.021
Li,Q.L.,Chen,F.K.,Yang,J.H.,et al.,2008.Single Grain Pyrite Rb-Sr Dating of the Linglong Gold Deposit,Eastern China.Ore Geology Reviews,34(3):263-270.https://doi.org/10.1016/j.oregeorev.2007.10.003
Li,S.H.,Zhang,J.,Deng,J.,et al.,2011.The Characteristics of Ore-Forming Fluid and Genetic Type of the Chang'an Gold Deposit in Southern Ailaoshan Metallogenic Belt.Acta Petrologica Sinica,27(12):3777-3786(in Chinese with English abstract).
Li,X.F.,Mao,J.W.,Wang,C.Z.,et al.,2007.The Daduhe Gold Field at the Eastern Margin of the Tibetan Plateau:He,Ar,S,O,and H Isotopic Data and Their Metallogenic Implications.Ore Geology Reviews,30(3-4):244-256.https://doi.org/10.1016/j.oregeorev.2005.10.005
Liang,Y.H.,Sun,X.M.,Shi,G.Y.,et al.,2011.Ore-Forming Fluid Geochemistry and Genesis of Laowangzhai Large Scale Orogenic Gold Deposit in Ailaoshan Gold Belt,Yunnan Province,China.Acta Petrologica Sinica,27(9):2533-2540(in Chinese with English abstract).
Lin,T.H.,Chung,S.L.,Chiu,H.Y.,et al.,2012.Zircon U-Pb and Hf Isotope Constraints from the Ailao Shan-Red River Shear Zone on the Tectonic and Crustal Evolution of Southwestern China.Chemical Geology,291(1):23-37.https://doi.org/10.1016/j.chemgeo.2011.11.011
Liu,J.J.,Liu,C.H.,Carranza,E.J.M.,et al.,2015a.Geological Characteristics and Ore-Forming Process of the Gold Deposits in the Western Qinling Region,China.Journal of Asian Earth Sciences,103:40-69.https://doi.org/10.1016/j.jseaes.2014.11.012
Liu,H.C.,Wang,Y.J.,Cawood,P.A.,et al.,2015b.Record of Tethyan Ocean Closure and Indosinian Collision along the Ailaoshan Suture Zone(SW China).Gondwana Research,27(3):1292-1306.https://doi.org/10.1016/j.gr.2013.12.013
Liu,W.,Fei,P.X.,2006.Methane-Rich Fluid Inclusions from Ophiolitic Dunite and Post-Collisional Mafic-Ultramafic Intrusion:The Mantle Dynamics underneath the PalaeoAsian Ocean through to the Post-Collisional Period.Earth and Planetary Science Letters,242(3-4):286-301.https://doi.org/10.1016/j.epsl.2005.11.059
MacKenzie,D.J.,Craw,D.,Begbie,M.,2007.Mineralogy,Geochemistry,and Structural Controls of a Disseminated Gold-Bearing Alteration Halo around the Schist-Hosted Bullendale Orogenic Gold Deposit,New Zealand.Journal of Geochemical Exploration,93(3):160-176.
Malpas,J.,Zhou,M.F.,Robinson,P.T.,et al.,2003.Geochemical and Geochronological Constraints on the Origin and Emplacement of the Yarlung Zangbo Ophiolites,Southern Tibet.Geological Society,London,Special Publications,218(1):191-206.https://doi.org/10.1144/gsl.sp.2003.218.01.11
Mao,J.W.,Pirajno,F.,Xiang,J.F.,et al.,2011.Mesozoic Molybdenum Deposits in the East Qinling-Dabie Orogenic Belt:Characteristics and Tectonic Settings.Ore Geology Reviews,43(1):264-293.https://doi.org/10.1016/j.oregeorev.2011.07.009
Mao,J.W.,Qiu,Y.M.,Goldfarb,R.J.,et al.,2002.Geology,Distribution,and Classification of Gold Deposits in the Western Qinling Belt,Central China.Mineralium Deposita,37(3-4):352-377.
Mao,J.W.,Wang,Y.T.,Li,H.M.,et al.,2008.The Relationship of Mantle-Derived Fluids to Gold Metallogenesis in the Jiaodong Peninsula:Evidence from D-O-C-S Isotope Systematics.Ore Geology Reviews,33(3-4):361-381.https://doi.org/10.1016/j.oregeorev.2007.01.003
Mao,J.W.,Xie,G.Q.,Li,X.F.,et al.,2004.Mesozoic Large Scale Mineralization and Multiple Lithospheric Extension in South China.Earth Science Frontiers,11(1):45-55(in Chinese with English abstract).
Mao,J.W.,Xie,G.Q.,Zhang,Z.H.,et al.,2005.Mesozoic Large-Scale Metallogenic Pulses in North China and Corresponding Geodynamic Settings.Acta Petrologica Sinica,21(1):169-188(in Chinese with English abstract).
McNaughton,N.J.,Groves,D.I.,Witt,W.K.,1993.The Source of Lead in Archaean Lode Gold Deposits of the Menzies-Kalgoorlie-Kambalda Region,Yilgarn Block,Western Australia.Mineralium Deposita,28(6):495-502.
Mernagh,T.P.,Bierlein,F.P.,2008.Transport and Precipitation of Gold in Phanerozoic Metamorphic Terranes from Chemical Modeling of Fluid-Rock Interaction.Economic Geology,103(8):1613-1640.https://doi.org/10.2113/gsecongeo.103.8.1613
Morelli,R.,Creaser,R.A.,Seltmann,R.,et al.,2007.Age and Source Constraints for the Giant Muruntau Gold Deposit,Uzbekistan,from Coupled Re-Os-He Isotopes in Arsenopyrite.Geology,35(9):795-798.
Müller,D.,Groves,D.I.,1997.Indirect Associations between Lamprophyres and Gold-Copper Deposits.In:Müller,D.,Groves,D.I.,eds.,Potassic Igneous Rocks and Associated Gold-Copper Mineralization.Springer,Berlin,Heidelberg,143-166.
Munro,M.A.,Ord,A.,Hobbs,B.E.,2018.Spatial Organization of Gold and Alteration Mineralogy in Hydrothermal Systems:Wavelet Analysis of Drillcore from Sunrise Dam Gold Mine,Western Australia.Geological Society,London,Special Publications,453(1):165-204.https://doi.org/10.1144/sp453.10
Nesbitt,B.E.,1991.Phanerozoic Gold Deposits in Tectonically Active Continental Margins.In:Nesbitt,B.E.,ed.,Gold Metallogeny and Exploration.Springer,Boston,MA,104-132.
Peacock,S.A.,1990.Fluid Processes in Subduction Zones.Science,248(4953):329-337.https://doi.org/10.1126/science.248.4953.329
Peacock,S.M.,Christensen,N.I.,Bostock,M.G.,et al.,2011.High Pore Pressures and Porosity at 35 km Depth in the Cascadia Subduction Zone.Geology,39(5):471-474.https://doi.org/10.1130/g31649.1
Phillips,G.N.,Powell,R.,1993.Link between Gold Provinces.Economic Geology,88(5):1084-1098.https://doi.org/10.2113/gsecongeo.88.5.1084
Phillips,G.N.,Powell,R.,2009.Formation of Gold Deposits:Review and Evaluation of the Continuum Model.EarthScience Reviews,94(1-4):1-21.https://doi.org/10.1016/j.earscirev.2009.02.002
Phillips,G.N.,Powell,R.,2010.Formation of Gold Deposits:A Metamorphic Devolatilization Model.Journal of Metamorphic Geology,28(6):689-718.
Phillips,G.N.,Powell,R.,2015.A Practical Classification of Gold Deposits,with a Theoretical Basis.Ore Geology Reviews,65:568-573.https://doi.org/10.1016/j.oregeorev.2014.04.006
Pili,é.,Kennedy,B.M.,Conrad,M.E.,et al.,2011.Isotopic Evidence for the Infiltration of Mantle and Metamorphic CO2-H2O Fluids from below in Faulted Rocks from the San Andreas Fault System.Chemical Geology,281(3-4):242-252.https://doi.org/10.1016/j.chemgeo.2010.12.011
Pitcairn,I.K.,Craw,D.,Teagle,D.A.H.,2015.Metabasalts as Sources of Metals in Orogenic Gold Deposits.Mineralium Deposita,50(3):373-390.doi:10.1007/s00126-014-0547-y
Pitcairn,I.K.,Teagle,D.A.H.,Craw,D.,et al.,2006.Sources of Metals and Fluids in Orogenic Gold Deposits:Insights from the Otago and Alpine Schists,New Zealand.Economic Geology,101(8):1525-1546.https://doi.org/10.2113/gsecongeo.101.8.1525
Ridley,J.R.,Diamond,L.W.,2000.Fluid Chemistry of Orogenic Lode Gold Deposits and Implications for Genetic Models.Reviews in Economic Geology,13:141-162.
Romer,R.L.,Kroner,U.,2018.Paleozoic Gold in the Appalachians and Variscides.Ore Geology Reviews,92:475-505.https://doi.org/10.1016/j.oregeorev.2017.11.021
Rospabé,M.,Ceuleneer,G.,Benoit,M.,et al.,2017.Origin of the Dunitic Mantle-Crust Transition Zone in the Oman Ophiolite:The Interplay between Percolating Magmas and High-Temperature Hydrous Fluids.Geology,45(5):471-474.https://doi.org/10.1130/g38778.1
Saager,R.,Meyer,M.,Muff,R.,1982.Gold Distribution in Supracrustal Rocks from Archean Greenstone Belts of Southern Africa and from Paleozoic Ultramafic Complexes of the European Alps;Metallogenic and Geochemical Implications.Economic Geology,77(1):1-24.https://doi.org/10.2113/gsecongeo.77.1.1
Sack,P.J.,Large,R.R.,Gregory,D.D.,2018.Geochemistry of Shale and Sedimentary Pyrite as a Proxy for Gold Fertility in the Selwyn Basin Area,Yukon.Mineralium Deposita,53(7):997-1018.https://doi.org/10.1007/s00126-018-0793-5
Safonov,Y.G.,2010.Topical Issues of the Theory of Gold Deposit Formation.Geology of Ore Deposits,52(6):438-458.
Sarma,D.S.,Fletcher,I.R.,Rasmussen,B.,et al.,2011.Archaean Gold Mineralization Synchronous with Late Cratonization of the Western Dharwar Craton,India:2.52 Ga U-Pb Ages of Hydrothermal Monazite and Xenotime in Gold Deposits.Mineralium Deposita,46(3):273-288.
Sausse,J.,Jacquot,E.,Fritz,B.,et al.,2001.Evolution of Crack Permeability during Fluid-Rock Interaction.Example of the Brézouard Granite(Vosges,France).Tectonophysics,336(1-4):199-214.https://doi.org/10.1016/s0040-1951(01)00102-0
Schrauder,M.,Navon,O.,1994.Hydrous and Carbonatitic Mantle Fluids in Fibrous Diamonds from Jwaneng,Botswana.Geochimica et Cosmochimica Acta,58(2):761-771.https://doi.org/10.1016/0016-7037(94)90504-5
Selvaraja,V.,Caruso,S.,Fiorentini,M.L.,et al.,2017.Atmospheric Sulfur in the Orogenic Gold Deposits of the Archean Yilgarn Craton,Australia.Geology,45(8):691-694.
Seno,T.,Kirby,S.H.,2014.Formation of Plate Boundaries:The Role of Mantle Volatilization.Earth-Science Reviews,129:85-99.https://doi.org/10.1016/j.earsciev.2013.10.011
Sibson,R.H.,1996.Structural Permeability of Fluid-Driven Fault-Fracture Meshes.Journal of Structural Geology,18(8):1031-1042.https://doi.org/10.1016/0191-8141(96)00032-6
Sibson,R.H.,2001.Seismogenic Framework for Ore Deposition.Reviews in Economic Geology,14:25-50.
Sibson,R.H.,2004.Controls on Maximum Fluid Overpressure Defining Conditions for Mesozonal Mineralisation.Journal of Structural Geology,26(6-7):1127-1136.https://doi.org/10.1016/j.jsg.2003.11.003
Sibson,R.H.,2013.Stress Switching in Subduction Forearcs:Implications for Overpressure Containment and Strength Cycling on Megathrusts.Tectonophysics,600:142-152.https://doi.org/10.1016/j.tecto.2013.02.035
Sibson,R.H.,Robert,F.,Poulsen,K.H.,1988.High-Angle Reverse Faults,Fluid-Pressure Cycling,and Mesothermal Gold-Quartz Deposits.Geology,16(6):551-555.
Sibson,R.H.,Scott,J.,1998.Stress/Fault Controls on the Containment and Release of Overpressured Fluids:Examples from Gold-Quartz Vein Systems in Juneau,Alaska;Victoria,Australia and Otago,New Zealand.Ore Geology Reviews,13(1-5):293-306.https://doi.org/10.1016/s0169-1368(97)00023-1
Sillitoe,R.H.,1991.Intrusion-Related Gold Deposits.In:Sillitoe,R.H.,ed.,Gold Metallogeny and Exploration.Springer,Boston,MA,165-209.
Sillitoe,R.H.,2008.Major Gold Deposits and Belts of the North and South American Cordillera:Distribution,Tectonomagmatic Settings,and Metallogenic Considerations.Economic Geology,103(4):663-687.
Sillitoe,R.H.,Thompson,J.F.H.,1998.Intrusion-Related Vein Gold Deposits:Types,Tectono-Magmatic Settings and Difficulties of Distinction from Orogenic Gold Deposits.Resource Geology,48(4):237-250.https://doi.org/10.1111/j.1751-3928.1998.tb00021.x
Song,Y.,Jiang,S.H.,Bagas,L.,et al.,2016.The Geology and Geochemistry of Jinchangyu Gold Deposit,North China Craton:Implications for Metallogenesis and Geodynamic Setting.Ore Geology Reviews,73:313-329.https://doi.org/10.1016/j.oregeorev.2014.10.031
Spence-Jones,C.P.,Jenkin,G.R.T.,Boyce,A.J.,et al.,2018.Tellurium,Magmatic Fluids and Orogenic Gold:An Early Magmatic Fluid Pulse at Cononish Gold Deposit,Scotland.Ore Geology Reviews,102:894-905.https://doi.org/10.1016/j.oregeorev.2018.05.014
Standish,C.D.,Dhuime,B.,Chapman,R.J.,et al.,2014.The Genesis of Gold Mineralisation Hosted by Orogenic Belts:A Lead Isotope Investigation of Irish Gold Deposits.Chemical Geology,378-379:40-51.https://doi.org/10.1016/j.chemgeo.2014.04.012
Steadman,J.A.,Large,R.R.,2016.Synsedimentary,Diagenetic,and Metamorphic Pyrite,Pyrrhotite,and Marcasite at the Homestake BIF-Hosted Gold Deposit,South Dakota,USA:Insights on Au-As Ore Genesis from Textural and LA-ICP-MS Trace Element Studies.Economic Geology,111(7):1731-1752.https://doi.org/10.2113/econgeo.111.7.1731
Steadman,J.A.,Large,R.R.,Meffre,S.,et al.,2013.Age,Origin and Significance of Nodular Sulfides in 2 680 Ma Carbonaceous Black Shale of the Eastern Goldfields Superterrane,Yilgarn Craton,Western Australia.Precambrian Research,230:227-247.https://doi.org/10.1016/j.precamres.2013.02.013
Streit,J.E.,Cox,S.F.,2001.Fluid Pressures at Hypocenters of Moderate to Large Earthquakes.Journal of Geophysical Research:Solid Earth,106(B2):2235-2243.https://doi.org/10.1029/2000jb900359
Stüwe,K.,1998.Heat Sources of Cretaceous Metamorphism in the Eastern Alps:A Discussion.Tectonophysics,287(1-4):251-269.https://doi.org/10.1016/s0040-1951(98)80072-3
Sun,X.M.,Wei,H.X.,Zhai,W.,et al.,2014.Bangbu:The Largest Cenozic Orogenic Gold Deposit in Southern Tibet,China.Acta Geologica Sinica(English Edition),88(Suppl.2):788-789.
Sun,X.M.,Wei,H.X.,Zhai,W.,et al.,2016.Fluid Inclusion Geochemistry and Ar-Ar Geochronology of the Cenozoic Bangbu Orogenic Gold Deposit,Southern Tibet,China.Ore Geology Reviews,74:196-210.https://doi.org/10.1016/j.oregeorev.2015.11.021
Sun,X.M.,Zhang,Y.,Xiong,D.X.,et al.,2009.Crust and Mantle Contributions to Gold-Forming Process at the Daping Deposit,Ailaoshan Gold Belt,Yunnan,China.Ore Geology Reviews,36(1-3):235-249.https://doi.org/10.1016/j.oregeorev.2009.05.002
Tang,J.,Zheng,Y.F.,Wu,Y.B.,et al.,2007.Geochronology and Geochemistry of Metamorphic Rocks in the Jiaobei Terrane:Constraints on Its Tectonic Affinity in the Sulu Orogen.Precambrian Research,152(1-2):48-82.https://doi.org/10.1016/j.precamres.2006.09.001
Tang,L.,Santosh,M.,2018.Neoarchean Granite-Greenstone Belts and Related Ore Mineralization in the North China Craton:An Overview.Geoscience Frontiers,9(3):751-768.
Tomkins,A.G.,2010.Windows of Metamorphic Sulfur Liberation in the Crust:Implications for Gold Deposit Genesis.Geochimica et Cosmochimica Acta,74(11):3246-3259.https://doi.org/10.1016/j.gca.2010.03.003
Tomkins,A.G.,Grundy,C.,2009.Upper Temperature Limits of Orogenic Gold Deposit Formation:Constraints from the Granulite-Hosted Griffin's Find Deposit,Yilgarn Craton.Economic Geology,104(5):669-685.https://doi.org/10.2113/gsecongeo.104.5.669
Tripp,G.I.,Vearncombe,J.R.,2004.Fault/fracture Density and Mineralization:A Contouring Method for Targeting in Gold Exploration.Journal of Structural Geology,26(6-7):1087-1108.https://doi.org/10.1016/j.jsg.2003.11.002
Vearncombe,J.R.,1998.Shear Zones,Fault Networks,and Archean Gold.Geology,26(9):855.
Wall,V.J.,Graupner,T.,Yantsen,V.,et al.,2004.Muruntau,Uzbekistan:A Giant Thermal Aureole Gold(TAG)System.In:Muhling,J.,Goldfarb,R.,Vielreicher,N.,et al.,eds.,SEG 2004:Predictive Mineral Discovery Under Cover:Extended Abstracts:Centre for Global Metallogeny.University of Western Australia Publication,Perth,Australia,199-203.
Wang,C.S.,Liu,Z.F.,Hébert,R.,2000.The Yarlung-Zangbo Paleo-Ophiolite,Southern Tibet:Implications for the Dynamic Evolution of the Yarlung-Zangbo Suture Zone.Journal of Asian Earth Sciences,18(6):651-661.
Wang,Q.F.,Deng,J.,Groves,D.I.,Ore-Controlling Structure and Genesis of Orogenic Gold Deposit with Evolving Orogenesis:Case Study from Miocene Ailaoshan Orogenic Gold Deposits,TibetSoutheastern.Mineralium Deposita(in review).
Wang,Q.F.,Deng,J.,Liu,H.,et al.,2010a.Fractal Models for Ore Reserve Estimation.Ore Geology Reviews,37(1):2-14.https://doi.org/10.1016/j.oregeorev.2009.11.002
Wang,Q.F.,Deng,J.,Zhao,J.,et al.,2010b.Tonnage-Cutoff Model and Average Grade-Cutoff Model for a Single Ore Deposit.Ore Geology Reviews,38(1-2):113-120.https://doi.org/10.1016/j.oregeorev.2010.07.003
Wang,R.,Richards,J.P.,Zhou,L.M.,et al.,2015b.The Role of Indian and Tibetan Lithosphere in Spatial Distribution of Cenozoic Magmatism and Porphyry Cu-Mo Deposits in the Gangdese Belt,Southern Tibet.Earth-Science Reviews,150:68-94.
Wang,X.M.,Shao,S.C.,Wang,D.B.,2000.The Features and Geological Significance of Inclusion and Hydrogen and Oxygen Isotopes in Western Qinling Area.Journal of Precious Metallic Geology:9(1):44-48(in Chinese with English abstract).
Wang,Y.J.,Fan,W.M.,Zhang,G.W.,et al.,2013.Phanerozoic Tectonics of the South China Block:Key Observations and Controversies.Gondwana Research,23(4):1273-1305.https://doi.org/10.1016/j.gr.2012.02.019
Wang,Z.L.,Yang,L.Q.,Guo,L.N.,et al.,2015a.Fluid Immiscibility and Gold Deposition in the Xincheng Deposit,Jiaodong Peninsula,China:A Fluid Inclusion Study.Ore Geology Reviews,65:701-717.https://doi.org/10.1016/j.oregeorev.2014.06.006
Weatherley,D.K.,Henley,R.W.,2013.Flash Vaporization during Earthquakes Evidenced by Gold Deposits.Nature Geoscience,6(4):294-298.https://doi.org/10.1038/ngeo1759
Webber,A.P.,Roberts,S.,Taylor,R.N.,et al.,2013.Golden Plumes:Substantial Gold Enrichment of Oceanic Crust during Ridge-Plume Interaction.Geology,41(1):87-90.https://doi.org/10.1130/g33301.1
Weinberg,R.F.,Hodkiewicz,P.F.,Groves,D.I.,2004.What Controls Gold Distribution in Archean Terranes?Geology,32(7):545-548.https://doi.org/10.1130/g20475.1
Weller,O.M.,St-Onge,M.R.,Waters,D.J.,et al.,2013.Quantifying Barrovian Metamorphism in the Danba Structural Culmination of Eastern Tibet.Journal of Metamorphic Geology,31(9):909-935.https://doi.org/10.1111/jmg.12050
Whitney,D.L.,Teyssier,C.,Fayon,A.K.,2004.Isothermal Decompression,Partial Melting and Exhumation of Deep Continental Crust.Geological Society,London,Special Publications,227(1):313-326.https://doi.org/10.1144/gsl.sp.2004.227.01.16
Williams,H.M.,Turner,S.P.,Kelley,S.,et al.,2001.Age and Composition of Dikes in Southern Tibet:New Constraints on the Timing of East-West Extension and Its Relationship to Postcollisional Volcanism.Geology,29(4):339-342.
Williams,H.M.,Turner,S.P.,Pearce,J.A.,et al.,2004.Nature of the Source Regions for Post-Collisional,Potassic Magmatism in Southern and Northern Tibet from Geochemical Variations and Inverse Trace Element Modelling.Journal of Petrology,45(3):555-607.
Williams-Jones,A.E.,Bowell,R.J.,Migdisov,A.A.,2009.Gold in Solution.Elements,5(5):281-287.
Wintsch,R.P.,Christoffersen,R.,Kronenberg,A.K.,1995.Fluid-Rock Reaction Weakening of Fault Zones.Journal of Geophysical Research:Solid Earth,100(B7):13021-13032.https://doi.org/10.1029/94jb02622
Wyman,D.A.,1989.Archean Shoshonitic Lamprophyres Associated with Superior Province Gold Deposits:Distribution,Tectonic Setting,Noble Metal Abundances,and Significance for Gold Mineralization.Economic Geology Monographs,6:661-667.
Wyman,D.A.,Kerrich,R.,2010.Mantle Plume-Volcanic Arc Interaction:Consequences for Magmatism,Metallogeny,and Cratonization in the Abitibi and Wawa Subprovinces,Canada.Canadian Journal of Earth Sciences,47(5):565-589.https://doi.org/10.1139/e09-049
Wyman,D.A.,O’Neill,C.O.,Ayer,J.A.,2008.Evidence for Modern-Style Subduction to 3.1 Ga:A Plateau-AdakiteGold(Diamond)Association.The Geological Society of America,440:129-148.
Yang,J.H.,Wu,F.Y.,Wilde,S.A.,2003.A Review of the Geodynamic Setting of Large-Scale Late Mesozoic Gold Mineralization in the North China Craton:An Association with Lithospheric Thinning.Ore Geology Reviews,23(3-4):125-152.https://doi.org/10.1016/s0169-1368(03)00033-7
Yang,L.,Wang,Q.F.,Liu,X.F.,2015.Correlation between Mineralization Intensity and Fluid-Rock Reaction in the Xinli Gold Deposit,Jiaodong Peninsula,China:Constraints from Petrographic and Statistical Approaches.Ore Geology Reviews,71:29-39.https://doi.org/10.1016/j.oregeorev.2015.04.005
Yang,L.,Wang,Q.F.,Wang,Y.N.,et al.,2018b.Proto-to Paleo-Tethyan Evolution of the Eastern Margin of Simao Block.Gondwana Research,62:61-74.https://doi.org/10.1016/j.gr.2018.02.012
Yang,L.,Zhao,R.,Wang,Q.F.,et al.,2018a.Fault Geometry and Fluid-Rock Reaction:Combined Controls on Mineralization in the Xinli Gold Deposit,Jiaodong Peninsula,China.Journal of Structural Geology,111:14-26.https://doi.org/10.1016/j.jsg.2018.03.009
Yang,L.Q.,Deng,J.,Guo,C.Y.,et al.,2009a.Ore-Forming Fluid Characteristics of the Dayingezhuang Gold Deposit,Jiaodong Gold Province,China.Resource Geology,59(2):181-193.
Yang,L.Q.,Deng,J.,Guo,L.N.,et al.,2016a.Origin and Evolution of Ore Fluid,and Gold-Deposition Processes at the Giant Taishang Gold Deposit,Jiaodong Peninsula,Eastern China.Ore Geology Reviews,72:585-602.https://doi.org/10.1016/j.oregeorev.2015.08.021
Yang,L.Q.,Deng,J.,Wang,Z.L.,et al.,2016b.Thermochronologic Constraints on Evolution of the Linglong Metamorphic Core Complex and Implications for Gold Mineralization:A Case Study from the Xiadian Gold Deposit,Jiaodong Peninsula,Eastern China.Ore Geology Reviews,72:165-178.https://doi.org/10.1016/j.oregeorev.2015.07.006
Yang,L.Q.,Deng,J.,Wang,Z.L.,et al.,2016c.Relationships between Gold and Pyrite at the Xincheng Gold Deposit,Jiaodong Peninsula,China:Implications for Gold Source and Deposition in a Brittle Epizonal Environment.Economic Geology,111(1):105-126.https://doi.org/10.2113/econgeo.111.1.105
Yang,L.Y.,Yang,L.Q.,Yuan,W.M.,et al.,2013.Origin and Evolution of Ore Fluid for Orogenic Gold Traced by D-O Isotopes:A Case from the Jiapigou Gold Belt,China.Acta Petrologica Sinica,29(11):4025-4035.
Yang,Q.Y.,Santosh,M.,2015.Paleoproterozoic Arc Magmatism in the North China Craton:No Siderian Global Plate Tectonic Shutdown.Gondwana Research,28(1):82-105.
Yang,Z.S.,Hou,Z.Q.,Meng,X.J.,et al.,2009b.Post-Collisional Sb and Au Mineralization Related to the South Tibetan Detachment System,Himalayan Orogen.Ore Geology Reviews,36(1-3):194-212.
Yasuhara,H.,Polak,A.,Mitani,Y.,et al.,2006.Evolution of Fracture Permeability through Fluid-Rock Reaction under Hydrothermal Conditions.Earth and Planetary Science Letters,244(1-2):186-200.
Zhai,M.G.,Peng,P.,2007.Paleoproterozoic Events in the North China Craton.Acta Petrologica Sinica,23(11):2665-2682(in Chinese with English abstract).
Zhai,W.,Sun,X.M.,Yi,J.Z.,et al.,2014.Geology,Geochemistry,and Genesis of Orogenic Gold-Antimony Mineralization in the Himalayan Orogen,South Tibet,China.Ore Geology Reviews,58:68-90.https://doi.org/10.1016/j.oregeorev.2013.11.001
Zhai,Y.S.,Wang,J.P.,Peng,R.M.,et al.,2009.Research on Superimposed Metallogenic Systems and Polygenetic Mineral Deposits.Earth Science Frontiers,16(6):282-290(in Chinese with English abstract).
Zhang,G.Y.,Zheng,Y.Y.,Zhang,J.F.,et al.,2011.Ore-Control Structural and Geochronologic Constrain in Shalagang Antimony Deposit in Southern Tibet,China.Acta Petrologica Sinica,27(7):2143-2149(in Chinese with English abstract).
Zhang,H.F.,Parrish,R.,Zhang,L.,et al.,2007.A-Type Granite and Adakitic Magmatism Association in SongpanGarze Fold Belt,Eastern Tibetan Plateau:Implication for Lithospheric Delamination.Lithos,97(3-4):323-335.https://doi.org/10.1016/j.lithos.2007.01.002
Zhang,L.,Chen,H.Y.,Chen,Y.J.,et al.,2012.Geology and Fluid Evolution of the Wangfeng Orogenic-Type Gold Deposit,Western Tian Shan,China.Ore Geology Reviews,49:85-95.https://doi.org/10.1016/j.oregeorv.2012.09.002
Zhang,L.C.,Shen,Y.C.,Ji,J.S.,2003.Characteristics and Genesis of Kanggur Gold Deposit in the Eastern Tianshan Mountains,NW China:Evidence from Geology,Isotope Distribution and Chronology.Ore Geology Reviews,23(1-2):71-90.https://doi.org/10.1016/s0169-1368(03)00016-7
Zhang,L.C.,Zhou,X.H.,Ding,S.J.,2008.Mantle-Derived Fluids Involved in Large-Scale Gold Mineralization,Jiaodong District,China:Constraints Provided by the He-Ar and H-O Isotopic Systems.International Geology Review,50(5):472-482.https://doi.org/10.2747/0020-6814.50.5.472
Zhao,H.S.,Wang,Q.F.,Groves,D.I.,et al.,2019.A Rare Phanerozoic Amphibolite-Hosted Gold Deposit at Danba,Yangtze Craton,China:Significance to Fluid and Metal Sources for Orogenic Gold Systems.Mineralium Deposita,54(1):133-152.https://doi.org/10.1007/s00126-018-0845-x
Zhong,R.C.,Brugger,J.,Tomkins,A.G.,et al.,2015.Fate of Gold and Base Metals during Metamorphic Devolatilization of a Pelite.Geochimica et Cosmochimica Acta,171:338-352.doi:10.1016/j.gca.2015.09.013
Zhou,M.F.,Yan,D.P.,Kennedy,A.K.,et al.,2002a.SHRIMP U-Pb Zircon Geochronological and Geochemical Evidence for Neoproterozoic Arc-Magmatism along the Western Margin of the Yangtze Block,South China.Earth and Planetary Science Letters,196(1-2):51-67.https://doi.org/10.1016/s0012-821x(01)00595-7
Zhou,T.H.,Goldfarb,R.J.,Phillips,N.G.,2002b.Tectonics and Distribution of Gold Deposits in China:An Overview.Mineralium Deposita,37(3):249-282.
Zhou,M.F.,Yan,D.P.,Vasconcelos,P.M.,et al.,2008.Structural and Geochronological Constraints on the TectonoThermal Evolution of the Danba Domal Terrane,Eastern Margin of the Tibetan Plateau.Journal of Asian Earth Sciences,33(5-6):414-427.https://doi.org/10.1016/j.jseaes.2008.03.003
Zhu,L.H.,Qi,X.X.,Peng,S.B.,Li,Z.Q.,2011.Evolution of Ore Forming Fluid of Daping Gold Deposit in Ailaoshan Tectonic Zone,Southeast Tibet.Acta Petrologica Sinica,27(11):3395-3408.
Zhu,Y.N.,Peng,J.T.,2015.Infrared Microthermometric and Noble Gas Isotope Study of Fluid Inclusions in Ore Minerals at the Woxi Orogenic Au-Sb-W Deposit,Western Hunan,South China.Ore Geology Reviews,65:55-69.https://doi.org/10.1016/j.oregeorev.2014.08.014
毕献武,胡瑞忠,何明友,1997.哀牢山金矿带主要金矿床成矿流体特征.矿物学报,17(4):435-441.
陈衍景,Pirajno,F.,赖勇,等,2004.胶东矿集区大规模成矿时间和构造环境.岩石学报,20(4):907-922.
陈衍景,翟明国,蒋少涌,2009.华北大陆边缘造山过程与成矿研究的重要进展和问题.岩石学报,25(11):2695-2726.
邓军,杨立强,王长明,2011.三江特提斯复合造山与成矿作用研究进展.岩石学报,27(9):2501-2509.
李华健,王庆飞,杨林,等,2017.青藏高原碰撞造山背景造山型金矿床:构造背景、地质及地球化学特征.岩石学报,33(7):2189-2201.
李士辉,张静,邓军,等,2011.哀牢山南段长安金矿床成矿流体特征及成因类型探讨.岩石学报,27(12):3777-3786.
梁业恒,孙晓明,石贵勇,等,2011.云南哀牢山老王寨大型造山型金矿成矿流体地球化学.岩石学报,27(9):2533-2540.
毛景文,谢桂青,李晓峰,等,2004.华南地区中生代大规模成矿作用与岩石圈多阶段伸展.地学前缘,11(1):45-55.
毛景文,谢桂青,张作衡,等,2005.中国北方中生代大规模成矿作用的期次及其地球动力学背景.岩石学报,21(1):169-188.
王学明,邵世才,汪东波,等,2000.西秦岭金矿床包裹体、氢氧同位素特征及其地质意义.贵金属地质,9(1):44-48.
翟明国,彭澎,2007.华北克拉通古元古代构造事件.岩石学报,23(11):2665-2682.
翟裕生,王建平,彭润民,等,2009.叠加成矿系统与多成因矿床研究.地学前缘,16(6):282-290.
张刚阳,郑有业,张建芳,等,2011.西藏沙拉岗锑矿控矿构造及成矿时代约束.岩石学报,27(7):2143-2149.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |