河南熊耳山西段银铅锌矿床成矿作用及找矿预测研究
|
摘要
本文简要叙述了熊耳山西段成矿区的区域地质、地球物理、地球化学背景；对熊耳山西段银铅锌多金属矿田的地层、构造、岩浆岩、地球物理、地球化学等矿田地质特征进行了总结,重点阐述了变质核杂岩的控岩控矿特征,通过对燕山期花岗岩的地质学、岩石学、岩石地球化学、微量元素及稀土元素等特征的研究,判断花岗岩为下地壳物质部分熔融的成因并经历了上部地壳物质的混染,利用稀土元素部分熔融数学定量模型进行了模拟,表明太华群经30%的部分熔融即可形成区内的燕山期花岗岩,本区花岗岩其构造环境为造山期后型；矿田地球物理特征方面重力低异常指示隐伏岩体的存在,激电异常能够较准确地指示银铅矿体的产状及矿化规模；地球化学特征表明本区处于成矿背景极佳的地球化学富集区,以寨凹岩体环形高温元素组合异常为中心,周边分布着东、北、南三个次级环形中低温元素组合异常中心；通过对铁炉坪、蒿坪沟、沙沟典型矿床的矿区地质特征、矿(化)体及矿体特征、矿石结构构造、成矿阶段、围岩蚀变的研究,本区银铅锌矿床的总体特征可概括为矿脉规模较大,单个矿体长度小,厚度薄,银品位较高,矿石结构构造较简单,成矿阶段可分为三个阶段,围岩蚀变以矿脉为中心对称发育,中心以硅化为主；矿床明显受地层、构造控制；主要成矿时间为燕山期且紧随Ⅰ型花岗岩侵入之后；矿床属中低温、低盐度、浅成矿床：矿石铅同位素、硫同位素、氢氧同位素均支持岩浆和大气水混合的观点；在系统总结了矿床勘查工作的基础上,形成了不同比例尺层次下的对预测区、靶区、矿脉进行勘查的矿床勘查模型；通过基于MRAS系统的银资源潜力评价分析,估算了全区银资源总量,并划分A类远景预测区1个,B类远景预测区2个,C类远景预测区1个
The dissertation briefly describes the regional geology, geophysical and geochemical background of western Xiong'er metallogenic province, summarizes the Ag-Pb-Zn polymetallic ore field geological characteristics of strata, structure, magma, geophysics and geochemistry etc. Especially expounds the rock and mineralization controlling characteristics of metamorphic core complex. After studying the Yanshanian period granite geology, petrology, rock geochemistry, trace and REE earth elements etc, making sure that the granite were formed by the partially melting of lower crust and then contaminated by upper crust. The REE partially melting mathematic quantitative model simulation showing that the Yanshanian period granite with post-orogenic type tectonic environment background comes from the30%melting of Taihua group rock. In geophysical aspect, gravity low anomalies indicates the existence of concealed rock bodies while IP anomalies accurately indicates the occurrence and mineralization scale of Ag-Pb ore bodies. In geochemical aspect, this region is in the excellent metallogenic background geochemical enrichment zone which centers on Zhaiwa rock annular high temperature element composite anomalies and revolve around by three secondary ring-shaped middle and low temperature element composite anomalies in east, north and south direction. By researching geological, mineralization, ore structure, metallogenic stage and wall rock alteration characteristics of typical deposits such as Tieluping, Haopinggou and Shagou, summarising that the Ag-Pb-Zn deposit general characteristics are larger veins, thin and shorter single ore body with higher Ag grade. The ore structure is relatively simple and the metallogenic stage can be divided into three stages. The wall rock alteration are symmetric development centers on veins with siliconization mainly. Deposite is obviously controlled by the geological structure and can be classed as low temperature, low salinity and hypabyssal deposite. The main metallogenic time is Yanshanian period with immediately after the I-type granite intrusion. The ore Pb, S, H and O isotope studying resultes all support magmatic and meteoric water mixture viewpoint. Based on system summary of the deposit exploration, building the prospecting models in this area. Through evaluation and studying the Ag resources potentiality based on MRAS system, estimation the Ag resource in this region, then proposing1A category target,2B category targets and1C category target.
The dissertation briefly describes the regional geology, geophysical and geochemical background of western Xiong'er metallogenic province, summarizes the Ag-Pb-Zn polymetallic ore field geological characteristics of strata, structure, magma, geophysics and geochemistry etc. Especially expounds the rock and mineralization controlling characteristics of metamorphic core complex. After studying the Yanshanian period granite geology, petrology, rock geochemistry, trace and REE earth elements etc, making sure that the granite were formed by the partially melting of lower crust and then contaminated by upper crust. The REE partially melting mathematic quantitative model simulation showing that the Yanshanian period granite with post-orogenic type tectonic environment background comes from the30%melting of Taihua group rock. In geophysical aspect, gravity low anomalies indicates the existence of concealed rock bodies while IP anomalies accurately indicates the occurrence and mineralization scale of Ag-Pb ore bodies. In geochemical aspect, this region is in the excellent metallogenic background geochemical enrichment zone which centers on Zhaiwa rock annular high temperature element composite anomalies and revolve around by three secondary ring-shaped middle and low temperature element composite anomalies in east, north and south direction. By researching geological, mineralization, ore structure, metallogenic stage and wall rock alteration characteristics of typical deposits such as Tieluping, Haopinggou and Shagou, summarising that the Ag-Pb-Zn deposit general characteristics are larger veins, thin and shorter single ore body with higher Ag grade. The ore structure is relatively simple and the metallogenic stage can be divided into three stages. The wall rock alteration are symmetric development centers on veins with siliconization mainly. Deposite is obviously controlled by the geological structure and can be classed as low temperature, low salinity and hypabyssal deposite. The main metallogenic time is Yanshanian period with immediately after the I-type granite intrusion. The ore Pb, S, H and O isotope studying resultes all support magmatic and meteoric water mixture viewpoint. Based on system summary of the deposit exploration, building the prospecting models in this area. Through evaluation and studying the Ag resources potentiality based on MRAS system, estimation the Ag resource in this region, then proposing1A category target,2B category targets and1C category target.
引文
Barnes HL 1979.Solubilities of ore minerals, in:Barnes HL(ed) Geochemistry of Hydrothermal Ore Deposits.2nd edition, New York:Wiley-interscience, 404-460
BartosPJ.1987. Quiruvilca, Peru:Mineral zoning and timing of wall-rock alteration relative to Cu-Pb-Zn-Ag vein-fill deposition. Economic Geology,82:1431-1452.
Bendezu R and Pontbote 1..2002. Late timing for high-sulf idation Cordilleran base metal lode and replacement deposits in porphyry-related districts:the case of Colquijirca, central Peru. Society for Geology Applied to Mineral (SGA) News 13,9-13.
Bendezu R, Page L, Spikings R, Pecskay Z, Fontbote L.2008. New 40Ar/39Ar alunite ages from the Colqui jirca district, Peru:evidence of a long period of magmatic SO2 degassing during formation of epi thermal Au-Ag and Cordilleran polymetallic ores. Mineralium Deposita,43(7):777-789.
Bendezu R and Fontbote L. 2009. Cordilleran Epithermal Cu-Zn-Pb-(Au-Ag) Mineralization in the Colquijirca District, Central Peru:Deposit-Scale Mineralogical Patterns. Economic Geology,104(7):905-944
Bonham-Cater GF.1994. Geographic information systems for geoscientists:modelling with GIS. Oxford:Pergamon Press,398.
Boorder H, Spakman W, White SHetal.1998. Late Cenozoic mineralization, orogenic collapse and slab detachment in the European Alpine Belt. Earth and Planetary Science Letters.,164:569-575
Bouabdellah M, BeaudoinG, Leach DL.2009. Genesis of the Assif El Mal Zn-Pb(Cu, Ag)vein deposit. An extension-related Mesozoic vein system in the High Atlas of Morocco. Structural, mineralogical, and geochemical evidence. Mineralium Deposita,44(6):689-704
Cabri LJ.1987. The mineralogy of precious metals:new developments and metallurgical implications. Canadian Mineralogist,25(1):1-7
Cabri LJ.1992. The distribution of trace precious metals in minerals and mineral products. Mineralogical Magazine,56(3):289-308
Chen YJ, Pirajno F and Sui YH.2004. Isotope geochemistry of the Tieluping silver deposit, Henan, China:A case study of orogenic silver deposits and related tectonic setting. Mineral ium Deposita.39:560-575
Chen YJ, Franco P and Sui YH.2005. Geology and D-O-C isotope systematics of the Tieluping silver deposit, Henan, China:Implications for Ore Genesis. Acta Geologica Sinica,79(1):106-119
Chen YJ, Pirajno F, Qi JP.2008. The Shanggong gold deposit. Eastern Qinl ing Orogen, China:Isotope geochemistry and implications for ore genesis. Journal of Asian Earth Sciences,33(3-4):252-266
Cheng Guang-guo, Feng You-li, Yu Li-jing.2011. The application of GIS in management of mineral resources,20112nd International Conference on Artificial Intelligence, Management Science and Electronic Commerce,9:7317-7319
Costagliola P, Di Benedetto F, Banvenuti M, Bernardini GP, Cipriani C, Lattanzi PF, Romanelli M.2003. Chemical speciation of Ag in galena by EPR spectroscopy. American Mineralogist,88(8-9):1345-1350
Cox DP and Singer MA.1986. Mineral deposits models. U.S. Geological Survey Bulletin 1693:1-379
Creaser RA, Papanastassiou DA and Wasserburg GJ.1991. Negative thermal ion mass spectrometry of osmium, rhenium, and iridium. Geochim. Cosmochim. Acta.,55: 397-401
Einaudi MT.1982. General features and origin of skarns associated with porphyry copper plutons,In:Titley SR(ed.), Advance in geology of the porphyry copper deposits, Southwestern North America, University of Arizona Press, Tuscon, 185-209
Fan HR and Xie YH.1999. Porphyry-type molybdenum deposits in the eastern Qinling Mo belt, central China. Scientia Geologica Sinica,8(1):91-101
Foord EE, Shawe DR.1989. The Pb-Bi-Ag-Cu-(Hg)chemistry of galena and some associated sulfosalts:a review and some new data from Colorado, California and Pennsylvania. Canadian Mineralogist.27(3):363-382.
Gammons CH, Barnes HL.1989. The solubility of Ag2S in near-neutral aqueous sulf ide solutions at25 to 300 "C. Geochimica et Cosmochimica Acta,53(2):279-290
GaoS, Zhang BR, Jin ZM, Kern H, Luo TC and Zhao ZD.1998. How mafic is the lower continental crust? Earth and Planetary Science Letters,106:101-117
Gasparrini C.1984. The Mineralogy of Silver and Its Significance in Metal Extraction. Canadian Mining and Metallurgical Bulletin,77(866):99-110
Gasparrini C, Lowell GR.1985. Silver-bearing inclusions in "argentiferous" galena from the Silvermine district in southeastern Missouri. Canadian Mineralogist, 23(1):99-102
Gilbert JM and Park JR.1986. The geology of ore deposits. New York:Freeman and Co.,750
Giordano TH, Barnes HL.1979. Ore solution chemistry VI. PbS solubility in bisulfide solutions to 300℃. Economic Geology,74(7):1637-1646
Han YG, Zhang SH, Pirajno F, Wang Y, Zhang YH.2009. New 40Ar-39Ar age constraints on the deformation along the Machaoying fault zone:Implications for Early Cambrian tectonism in the North China Craton. Gondwana Research,16(2):255-263
Hayashi K, Sugaki A, Kitakaze A.1990. Solubility of sphalerite in aqueous sulfide solutions at temperatures between25 and240℃. Geochimica et Cosmochimica Acta, 54(3):715-725
He YH, Zhao GC, Sun M, Wilde SA.2008. Geochemistry, isotope systematics and petrogenesis of the volcanic rocks in the Zhongtiao Mountain:An alternative interpretation for the evolution of the southern margin of the North China Craton. Lithos,102(1-2):158-178
He YH, Zhao GC, Sun M, Han YG.2010. Petrogenesis and tectonic setting of volcanic rocks in the Xiaoshan and Waifangshan areas along the southern margin of the North China Craton:Constraints from bulk-rock geochemistry and Sr-Nd isotopic composition. Lithos,114(1-2):186-199
He YH, Zhao GC, Sun M, Xia Xiaoping.2009. SHRIMP and LA-ICP-MS zircon geochronology of the Xiong'er volcanic rocks:Implications for the Paleo-Mesoproterozoic evolution of the southern margin of the North China Craton. Precambrian Research,168(3-4):213-222.
Hedenquist JW, Arribas A, Reynolds TJ.1998. Evolution of an intrusion-centered hydrothermal system; Far Southeast-Lepanto porphyry and epithermal Cu-Au deposits, Philippines. Economic Geology,93(4):373-404
Hemley JJ and Hunt JP.1992. Hydrothermal ore-forming processes in the light of studies in rock-buffered systems:Ⅱ. Some general geologic applications. Economic Geology,87:23-43.
Henley RW and Ellis AJ.1983. Geothermal systems, ancient and modern. Earth Science Reviews,19:1-50
Hu HB, Mao JW, Liu DY, Niu SY, Wang YB, Li YF and Shi RR.2005. SHRIMP Zircon U-Pb Dating of the Tongshi Magmatic Complex in Western Shandong and Its Geological Implications. Acta Geologica Sinica,79(4):491-496
Jiang N, Xu JH, Song MX.1999. Fluid inclusion characteristics of mesothermal gold deposits in the Xiaoqinling district, Shaanxi and Henan Provinces, People's Republic of China. Mineralium Deposita,34(2):150-162
Kroner A, Composton W, Zhang GW, Guo AL, Todt W.1988. Age and tectonic setting of Late Archean greenstone-gneiss terrain in Henan Province, China, as revealed by single-grain zircon dating. Geology,16:211-215
Kusky TM, Windley BF, Zhai MG.2007. Tectonic evolution of the North China Block: from orogen to craton to orogen. Geolocial Society of London Special Publications,280:1-34
Li YF, Mao JW, Guo BJ, Shao YJ, Fei HC and Hu HB.2004. Re-Os isotopic dating of molybdenites in the Nannihu Mo (W) ore field in the east Qinling and Its Geodynamic processes. Acta Geologica Sinica,78(2):463-470
Leach DL, Bradley D, Lewchuk MT, Symons DT, de Marsily G, Brannon J.2001. Mississippi Valley-type lead-zinc deposits through geological time: implications from recent age-dating research. Mineralium Deposita,36(8): 711-740
Leach TM and Corbett GJ.1993. Porphyry-related carbonate-base metal gold systems: The transition between the epithermal and porphyry environments. In Second National Meeting Specialist Group in Economic Geology, Armidale, N. S.W., Geological Society of Australia Abstracts,34:39-40
Leach TM and Corbett GJ.1994. Porphyry-related carbonate-base-metal gold systems in the southwest Pacific:characteristics. In:Rogerson R(ed.), Geology, exploration and mining conference proceedings, Parkville, The Australasian Institute of Mining and Metallurgy,84-91
Lu SN, Zhao GC, Wang HC, Hao GJ.2008. Precambrian metamorphic basement and sedimentary cover of the North China Craton:A review. Precambrian Research, 160(1-2):77-93
Lueth VW, Megaw PKM, Pingitore NE.2000. Systematic variation in galena solid-solution compositions at Santa Eulalia, Chihuahua, Mexico. Economic Geology,95(8):1673-1678
Macfarlane AW and Petersen U.1990. Pb isotopes of the Hualgayoc area, northern Peru:Implications for metal provenance and genesis of a Cordilleran polymetallic mining district. Economic Geology,85:1303-1327.
Mao JW, Kerrich R, Li HY and Li YH.2002a. High Wife ratios in the Wangu gold deposit, Hunan Province, China:implications for mantle fluid along the Tanlu deep fault zone. Geochemical Journal,36(3):197-208
Mao JW, Wang YT, Ding TP, Chen YC, Wei JX and Yin JZ.2002b. Dashuigou Tellurium Deposit in Sichuan Province, China-An Example of Mantle Fluid Evolving in Mineralized Process:Evidences from C,0, H, S Isotopes. Resource Geology, 52(1):15-23
Mao JW, Goldfarb RJ, Zhang ZW, Xu WY, Qiu YM and Deng J.2002. Gold deposits in the Xiaoqinling-Xiong'ershan region. Qinling Mountains, central China. Mineralium Deposita,37:306-325
Mao JW, Li YQ, Goldfrab R, He Y and Zaw K.2003. Fluid inclusions noble gas studies of the Dongping gold deposit, Heibei Province, China:A mantle connection for mineralization. Economic Geology,98:517-534
Mao JW, Wang YT, Zhang ZH, Yu JJ, Niu BG.2003. Geodynamic settings of Mesozoic large-scale mineralization in North China and adjacent areas—Implication from the highly precise and accurate ages of metal deposits. Science in China (Series D),46(8):838-851
Mao JW, Xie GQ, Bierlein F, Qu WJ, Du AD, Ye HS, Pirajno F, Li HM, Guo BJ, Li YF, Yang ZQ.2008. Tectonic implications from Re-Os dating of Mesozoic molybdenum deposits in the East Qinling-Dabie orogenic belt. Geochimica et Cosmochimica Acta,72(18):4607-4626.
Merrihue C and turner G.1962. Potassium-argon dating by activation with fast neutrons. J. Geophys. Res,71:2852-2857
Mitchell AHG and Garson MS.1981. Mineral deposits and global tectonic settings. London:Academic Press,1-457
Pearce JA, Lippard SJ and Roberts S.1984. chteristics and tectonic significance of supra-subduction zone ophiolites. Marginal Basin Geology,16 (Geol Soc Spec Pub 1):77-93
Peng P, Zhai MG, Guo JH, Kusky T, Zhao TP.2007. Nature of mantle source contributions and crystal differentiation in the petrogenesis of the 1.78 Ga mafic dykes in the central North China craton. Gondwana Research,12(1-2):29-46
Peng P, Zhai MG, Ernst RE, Guo JH, Liu F, Hu B.2008. A 1.78 Ga large igneous province in the North China craton:The Xiong'er Volcanic Province and the North China dyke swarm. Lithos,101 (3-4):260-280
Ratschbacher L, Hacker BR, Andrew Calvert A, Webb LE, Grimmer JC, McWilliams MO, Ireland T, Dong SW and Hu JM.2003. Tectonics of the Qinl ing (Central China): tectonostratigraphy, geochronology, and deformation history. Tectonopysics, 366(1-2):1-53
Ruaya JR, Seward TM.1986. The stability of chlorozinc (Ⅱ)complexes in hydrothermal solutions up to 350℃. Geochimica et Cosmochimica Acta,50(5):651-661
Sawkins FJ.1984. Metal deposits in relation to plate tectonics. Springer-Verlag, Berlin, Heidelberg, New York, Tokyo,1-325
SawkinsFJ.1990. Metal Deposits in Relation to Plate Tectonics (2nd edition). Berlin: Springer-Verlag,1-461
Seward TM.1976. The stability of chloride complexes of silver in hydrothermal solutions up to 350℃. Geochimica et Cosmochimica Acta,40(11):1329-1341
Seward TM.1984. The formation of lead(Ⅱ)chloride complexes to 300℃:a spectrophotometric study. Geochimica et Cosmochimica Acta,48(1):121-134
Sharp TG and Buseck PR.1993. The distribution of Ag and Sb in galena:inclusions versus solid solution. American Mineralogist,78(1-2):85-95
Shirey SB and Walker RJ.1995. Carius tube digestion for low-blank rhenium-osmium analysis. Anal. Chem.,67:2136-2141
Stefansson, A. Seward, T. M.2003. Experimental determination of the stability and stoichiometry of sulphide complexes of silver(Ⅰ)in hydrothermal solutions to 400 ℃. Geochimica et Cosmochimica Acta,67(7):1395-1413
Stein HJ, Markey RJ, Morgan JW, Du A and Sun Y.1997. Highly precise and accurate Re-Os ages for molybdenite from the East Qinling molybdenum belt, Shanxi Province, China. Economic Geolology,92:827-835.
Sun X, Gong QJ, Wang QF, Yang LQ, Wang CM, Wang ZL.2010. Application of local singularity model to delineate geochemical anomalies in Xiong'ershan gold and molybdenum ore district, We stern Henan province, China. Journal of Geochemical Exploration,107(1):21-29
Suzuki K, Lu Q, Shimizu H, et al.1993. Reliable Re-Os age for molybdenite. Geochim. Cosmochim. Acta,57:1625-1628
Taylor SR and Mclennan SM.1985. The Continental Crust:its Composition and Evolution. BlackwelllScientific Publications, Oxford,312
Voudouris P, Melfos V, Spry PG.2008. Carbonate-replacement Pb-Zn-Ag ± Au mineralization in the Karnariza area, Lavrion, Greece:mineralogy and thermochemical conditions of formation. Mineralogy and Petrology,94(1-2): 85-106
Wan YS, Song B, Liu DY, Wilde SA, Wu JS, Yin XY, Zhou HY.2006. SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary rocks in the North China Craton:Evidence for a major Late Palaeoproterozoic tectonothermal event. Precambrian Research,149(3-4):249-271
Wang XL, Jiang SY, Dai BZ.2010. Melting of enriched Archean subcontinental lithospheric mantle:Evidence from the ca.1760 Ma volcanic rocks of the Xiong'er Group, southern margin of the North China Craton. Precambrian Research,182(3):204-216
Wilson JT, Static and mobile earth:The current scientific revolution in the earth. Proc. Am Phil. Soc.1968,112:309-320
Wyborn LAI, Valenta PK, Jagodzinski EA, Morse M, Wellman P.1989. Integration of Multiple geoscience data sets in the Coronation Hill region, NT, as an aid to delineate areas of potential mineralisation. BMR Research Symposium 1989.
Yang JH, Wu FY, Wilde SA.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
Zeng NS, Izawa E, Motomura Y, Lai LR.2000. Silver minerals and paragenesis in the Kangjiawan Pb-Zn-AgAu deposit of the Shuikoushan mineral district, Hunan Province, China.Canadian Mineralogist,38(1):11-22
Zhai MG, Liu WJ.2003. Palaeoproterozoic tectonic history of the North China craton: a review. Precambrian Research,122(1-4):183-199
Zhang DH, Xu GJ, Zhang WH, Golding SD.2007. High salinity fluid inclusions in the Yinshan polymetallic deposit from the Le-De metallogenic belt in Jiangxi Province, China:Their origin and implications for ore genesis. Ore Geology Reviews,31:247-260
Zhang SH, Li ZX, Wu HC.2006. New Precambrian palaeomagnetic constraints on the position of the North China Block in Rodinia. Precambrian Research, 144(3-4):213-238
Zhao GC, Sun M, Wilde SA, Li SZ.2003. Assembly, Accretion and Breakup of the Paleo-Mesoproterozoic Columbia Supercontinent:Records in the North China Craton. Gondwana Research,6(3):417-434
Zhao GC, Sun M, Wilde SA, Li SZ.2004. A Paleo-Mesoproterozoic supercontinent: assembly, growth and breakup. Earth-Science Reviews,67(1-2):91-123
Zhao GC, He YH, Sun M.2009. The Xiong'er volcanic belt at the southern margin of the North China Craton:Petrographic and geochemical evidence for its outboard position in the Paleo-Mesoproterozoic Columbia Supercontinent. Gondwana Research,16(2):170-181.
Zhao TP, Zhou MF.2009. Geochemical constraints on the tectonic setting of Paleoproterozoic A-type granites in the southern margin of the North China Craton. Journal of Asian Earth Sciences,36(2-3):183-195
Zhou TH, Goldfarb RJ, Phillips NG.2002. Tectonics and distribution of gold deposits in China-an overview. Minealimu Deposita,37(3-4):249-282
白凤军,赵太平,肖荣阁,刘国营.2010.河南嵩县钾长石石英脉型钼矿成矿流体地球化学.现代地质,24(1)：26-33
白瑾,戴风岩,颜耀阳.1997.中条山前寒武纪地壳演化.地学前缘,4(3-4)：281-289
包志伟,李创举,祁进平.2009.东秦岭铅锌银矿田辉长岩钻石SHRIMP铀-铅年龄及成矿时代.岩石学报,24(11)：2951-2956
曹荣,龙朱华寿.1995.地幔流体与成矿作用.地球科学进展,10(4)：324-329
曹烨,李胜荣,申俊峰,要梅娟,李庆康,毛付龙.2008.豫西前河构造蚀变岩型金矿成矿过程中的流体-岩石反应.矿床地质,27(6)：714-726
曹烨,李胜荣,申俊峰,要梅娟.2009.豫西前河金矿热液蚀变地球化学研究.中国地质,(1)：
陈江峰,谢智,刘顺生,李学明,K. A. Folan.1995.大别造山带冷却年龄的40Ar-39Ar和裂变径迹年龄测定.中国科学(B辑),25(10)：1086-1092
陈书中,狄卫民.2002.干树金矿V-#脉地质特征及成矿预测探讨.金属矿山,(4)：58-60
陈旺,郭时然.1994.河南洛宁蒿坪沟银铅金矿床地质特征.有色金属矿产与勘查,3(6)：336-341
陈旺.1995.豫西熊耳山金矿床和银(铅)矿床铅同位素研究.贵金属地质,4(3)：168-176
陈旺,郭时然,崔毫.1996.豫西熊耳山铁炉坪、蒿坪沟矿床银铅矿石稳定同位素研究.有色金属矿产与勘查,4(4)：213-218
陈伟军,刘红涛,张德会.2007.河北丰宁牛圈银矿床流体包裹体特征及地质意义.矿产与地质,21(1)：12-16
陈衍景,富士谷.1992.豫西金矿成矿规律.北京：地震出版社,1-188
陈衍景,隋颖慧,Franco PIRAJNO.2003.CMF模式的排他性依据和造山型银矿实例东秦岭铁炉坪银矿同位素地球化学.岩石学报,19(3)：551-568
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
陈毓川,朱裕生.1991.中国矿床成矿模式.北京：地质出版社,1-367
陈毓川.1994.矿床的成矿系列.地学前缘,1(4)：90-94
陈毓川,薛春纪,王登红,李华芹,路远发.2003.华北陆块北缘区域矿床成矿谱系探讨.高校地质学报,9(4)：520-535
程裕淇,陈毓川,赵一鸣.1979.初论矿床的成矿系列问题.中国地质科学院院报,第1号,1-55
程广国.1994.河南熊耳山地区中生代花岗岩成因及构造环境与成矿关系,有色金属矿产与勘查,1994(1)
程广国.1997.河南瑶沟金矿矿床地球化学特征及成矿预测模型模型,有色金属矿产与勘查,1997(2)
陈郑辉,陈毓川,王登红,等.2009.矿产资源潜力评价示范研究—以南岭东段钨矿资源潜力评价为例
戴宝章,蒋少涌,王孝磊.2009.河南东沟铝矿花岗斑岩成因：岩石地球化学、锆石U-Pb年代学及Sr-Nd-Hf同位素制约.岩石学报,25(11)：2889-2901
邓晋福,赵海玲,莫宣学.1996.中国大陆根-柱构造：大陆动力学的钥匙.北京：地质出版社,1-110
邓小华,陈衍景,姚军明,李文博,李诺,王运,糜梅,张颖.2008a.河南省洛宁县寨凹钼矿床流体包裹体研究及矿床成因.中国地质,35(6)：1250-1266
邓小华,李文博,李诺,糜梅,张颖.2008b.河南嵩县纸房钼矿床流体包裹体研究及矿床成因.岩石学报,24(9)：2133-2148
邓小华,姚军明,李晶.2009.东秦岭寨凹钼矿床辉钼矿Re-Os同位素年龄及熊耳期成矿事件.岩石学报,25(11)：2739-2746
邓亚婷,王北颖.1988.小秦岭小河岩体岩石谱系单位划分及其定位机制.陕西地质,16(2)：2-7
董有,彭万夫,乔怀栋,刘长命,冯祖钧,武跃诚.1983.豫西—洛南中酸性小岩体成钼地质条件的定量分析与统计预测模型.河南地质,1(2)：62-74
董有.1986.豫西—洛南斑岩铝矿带成岩成矿几个问题的探讨.河南地质,4(3)：14-20
杜安道,何红蓼,殷宁万,等.1994.辉钼矿的铼-锇同位素地质年龄测定方法研究.地质学报,68(4)：339-347
杜安道,赵敦敏,王淑贤,孙德忠,刘敦一.2001.Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄.岩矿测试,20(4)：247-252
杜乐天.1986b.碱交代作用的地球化学原理.中国科学(B),81-90
杜乐天.1988.幔汁H-A-C-O-N-S流体.大地构造与成矿学,12(1)：87-94
杜乐天.1989.幔汁(HACONS流体)的重大意义.大地构造与成矿学,13(1)：91-99
杜乐天.1990.幔汁(HACONS)假说.矿物岩石地球化学通讯,(1)：39-42
杜乐天.1996a.地壳流体与地幔流体问的关系.地学前缘,172-180
范宏瑞,谢奕汉,王英兰,赵瑞.1994.康山金矿地质地球化学特征及其成因.黄金,15(3)：1-6
范宏瑞,谢奕汉,郑学正,王英兰.2000.河南祁雨沟热液角砾岩体型金矿床成矿流体研究.岩石学报,16(4)：559-563
冯守忠,冯淼.2000.吉林山门银金矿床地质特征.贵金属地质,9(1)：15-19
高建京,毛景文,叶会寿,陈懋弘,郑榕芬.2010.豫西沙沟脉状Ag-Pb-Zn矿床地质特征和成矿流体研究.岩石学报,26(3)：740-756
高山,张本仁,金振民.1999.秦岭-大别造山带下地壳拆沉作用.中国科学,29(6)：532-541
耿元生,杨崇辉,宋彪,万渝生.2004.吕梁地区18亿年的后造山花岗岩：同位素年代和地球化学制约.高校地质学报,10(4)：477-487
贡二辰.2008.河南省洛宁县蒿坪沟银金多金属矿区地质特征及找矿方向分析.地质与勘探,44(1)：21-25
关保德,吕国芳,王耀霞.1993.河南省地台区中-晚元古代构造沉积盆地演化分析.河南地质,11(3)：181-190
郭保健,徐孟罗,王志光,戴塔根.1997.熊耳山北坡拆离断层带地球化学特征及其与金银矿化的关系.矿产与地质,11(1)：20-25
郭保健,李永峰,王志光,叶会寿.2005.熊耳山Au-Ag-Pb-Mo矿集区成矿模式与找矿方向.地质与勘探,41(5)：43-47
郭东升,陈衍景,祁进平.2007.河南祁雨沟金矿同位素地球化学和矿床成因分析.地质论评,53(2)：217-227
郭力宇,王树洗,赵东宏,陈有仓.1997.陕西洛南陶湾群三岔口组砾岩研究.地球学报,18(4)：352-357
郭奇斌.1992.从地球物理场特征谈河南地质构造.河南地质,10(4)：264-272
郭时然.1995.洛宁铁炉坪银铅矿床围岩蚀变分带特征.河南地质,13(1)：9-14
韩以贵,李向辉,张吐红,张元厚,陈福坤.2007.豫西祁雨沟金矿单颗粒和碎裂状黄铁矿Rb-Sr等时线定年.科学通报,52(11)：1307-1311
何红蓼,杜安道,邹晓秋,等.1993.铼-锇同位素的等离了体质谱测定及其在辉钼矿测年中的应用.岩矿测试,12(3)：161-165.
河南省地质矿产局.1989.河南省区域地质志.北京：地质出版社,1-722
何云龙,魏俊浩,谭文娟,李晶.2008.山西堡子湾隐爆角砾岩型金矿矿床隐爆机制研究.矿产与地质,22(5)：377-380
胡受奚,林潜龙,陈泽铭,等.1988.华北与华南古板块拼合带地质和成矿.南京：南京大学出版社,1-558
胡文瑄,孙睿,张文兰.2001.金矿成矿流体的特点及深-浅部流体相互作用成矿机制.地学前缘,8(4)：281-288
胡正国,钱壮志,阎广民,陈在劳,李民贤.1994.小秦岭拆离-变质核杂岩构造与金矿.西 安：陕西科学出版社,1-200
胡志宏,周顺之,胡受奚,陈泽铭.1986.豫西太华岩群混合岩特征及其与金钼矿化的关系.矿床地质,5(4)：71-81
胡志宏,胡受奚,周顺之.1990.东秦岭燕山期大陆内部挤压-俯冲背景的A型孪生花岗岩带.岩石学报,(1)：1-12
华仁民,陈培荣,张文兰,姚军明,林锦富,张展适,顾晟彦.2005.南岭与中生代花岗岩类有关的成矿作用及其大地构造背景.高校地质学报,11(3)：291-304
黄楚秀,黄建军.1985.小秦岭地区中生代花岗岩类成因系列及其与成矿关系.河南地质,3(增刊)：123-128
黄典豪,王义昌,聂凤军,江秀杰.1984.黄龙铺碳酸盐脉型钼(铅)矿矿床的硫、碳、氧同位素组成及成矿物质来源.地质学报,58(3)：252-264
黄典豪,王义昌,聂凤军,江秀杰.1985.一种新的钼矿床类型—陕西黄龙铺碳酸盐脉型钼(铅)矿矿床地质特征及成矿机制.地质学报,59(3)：241-257
黄典豪,吴澄宇,聂凤军.1987.陕西金堆城斑岩钼矿床地质特征及成因探讨.矿床地质,6(3)：22-34
黄典豪,董群英,甘志贤.1989.中国钼矿床.宋叔和主编,中国矿床.北京：地质出版社,482-512
黄典豪,吴澄宇,杜安道,等.1994.东秦岭地区钼矿床的铼-锇同位素年龄及其意义.矿床地质,13(3)：221-230
黄典豪,杜安道,吴澄宇,刘兰笙,孙亚莉,邹晓秋.1996.华北地台钼(铜)矿床成矿年代学研究.矿床地质,15(4)：365-373
黄凡,罗照华,卢欣祥,高飞,陈必河,杨宗锋,潘颖,李德东.2009.东沟含钼斑岩由太山庙岩基派生?矿床地质,(5)：569-584
黄建军,黄楚秀.1985.陕西小秦岭地区钼的区域地球化学场的分布特征与矿化关系.河南地质,3(增刊)：128-134
贾承造,施央申.1986.东秦岭燕山期A型板块俯冲带的研究.南京大学学报,22(1)：120-128
黎世美,曹庆臻,吴国昌.1985.河南栾川上房沟夕卡岩—斑岩型钼(铁)矿床的围岩蚀变与矿化特征.河南地质,3(增刊)：259-266
黎世美,瞿伦全,李新民,等.1993.熊耳山地区蚀变构造岩型金矿成矿地质条件富集规律成矿模式及远景预测.北京：地质出版社,96-132
黎世美,瞿伦全,苏振邦,黄建军,王小生,岳铮生.1996.小秦岭金矿地质和成矿预测.北京：地质出版社,57-174
李立,杨辟元,段波,李艳军,金国元,钟清,刘玉华,万明浩,高平.1998.东秦岭岩石层的地电模型.地球物理报,41(2)：189-196
李红艳,毛景文,孙亚莉,邹晓秋,何红蓼,杜安道.1996.柿竹园钨多金属矿床的Re-Os同位素等时线年龄研究.地质论评,42(3)：261-267
李厚民,王登红,张冠,陈毓川,王彦斌,张长青,代军治.2007.河南白石坡银矿区花岗斑岩中锆石的SHRIMP U-Pb年龄及其地质意义.地质学报,81(6)：808-813
李厚民,叶会寿,王登红,陈毓川,屈文俊,杜安道.2009.豫西熊耳山寨凹钼矿床辉钼矿铼-锇年龄及其地质意义.矿床地质,(2)：133-142
李济营,张云政,瓮纪昌,吕伟庆.2010.河南汝阳东沟钼矿床下铺花岗斑岩体特征及其控矿作用.地质调查与研究,33(3)：
李晶,陈衍景,李强之,唐国军.2004.东秦岭上宫金矿流体成矿作用：矿物学研究.矿物岩石,24(3)：28-35
李莉,齐金忠.2002.河南公峪石英脉型金矿地质特征及其成因探讨.矿床地质,21卷增刊：
李诺,孙亚莉,李晶,薛良伟,2008a.小秦岭大湖金钼矿床辉钼矿铼锇同位素年龄及印支期成矿事件.岩石学报,24(4)：810-816
李诺,赖勇,鲁颖淮,郭东升.2008b.河南祁雨沟金矿流体包裹体及矿床成因类型研究.35(6)：1230-1239
李诺,陈衍景,孙亚莉,胡海珠,李晶,张辉.2009.河南鱼池岭钼矿床辉钼矿铼-锇同位素年龄及地质意义.岩石学报,25(2)：413-421
李齐,王瑜,万景林,李大明,王非.2001.秦岭造山带中段中新生代构造抬升的热年代学证据.矿物岩石地球化学通报,20(4)：263-265
李三忠,刘建忠,赵国春,吴福元,韩宗珠,杨中柱.2004.华北克拉通东部地块中生代变形的关键时限及其对构造的制约-以胶辽地区为例.岩石学报,20(3)：633-646
李曙光,Hart S R,郭安林,等.1987.河南中部登封群全岩Sm-Nd同位素年龄及其构造意义.科学通报,(22)：1728-1731
李树臣,周利霞.2008.山西省灵丘县支家地铅锌银矿床地质特征及成矿预测.地质与勘探,44(3)：18-21
李先梓,严阵,卢欣祥.1993.大秦-大别山花岗岩.北京：地质出版社,1-216
李祥才,董绍忠,张志伟,马建德.2001.万银坑银多金属矿地质特征及成因探讨.有色矿冶,17(6)：1-4
李永峰,毛景文,白凤军,李俊平,和志军.2003.东秦岭南泥湖钼矿Re-Os同位素年龄及其地质意义.地质论评,49(6)：652-659
李永峰,毛景文,郭保健,白凤军.2004.豫西公峪金矿床地质地球化学特征及成因探讨.矿床地质,23(1)：61-66
李永峰,毛景文,胡华斌,白凤军,李厚民,李蒙文,郭保健,叶会寿.2005.豫西公峪金矿床流体包裹体及其He.Ar.S.H.O同位素组成对成矿流体来源的示踪.岩石学报,21(5):1347-1358
李永峰,毛景文,刘敦一,王彦斌,王志良,王义天,李晓峰,张作衡,郭保健.2006.豫西雷门沟斑岩钼矿SHRIMP锆石U-Pb及辉钼矿Re-Os测年及其地质意义.地质论评,52(1)：122-131
李振国,年平国.2009.河南省罗山县白石坡银多金属矿床地质特征及成矿规律分析.现代矿业,(5)：85-87
李志昌等.1988.衫-钕法实验条件研究和地质应用.中国地质科学院宜昌地质矿产研究所所刊,第13号,1-23
梁钢.1995.江西万年虎家尖银金矿床地质特征及矿床成因初探.江西地质,9(1)：52-61
刘敦一.2002.SHRIMP技术及其在中国的首次登陆.地质通报,21(1)：53
刘国惠,张寿广,游振东,等.1993.秦岭造山带主要变质岩群及其变质演化.北京：地质出版社,26-84
刘国营,刘国庆.2009.青岗坪金矿床地质特征及成因探讨.桂林工学院学报,29(3)：323-326
刘灵恩,胡国民,支凤歧.2004.豫西寨凹隐伏岩体对周边银多金属矿的控矿作用.矿产与地质,18(1)：31-34
刘灵恩,王永争,刘金平.2011.矿化率在商业性地质勘查开发中的应用探讨.矿产勘查,待刊
刘灵恩,翟东兴,李红超,张侍威.2011.豫西沙沟-月亮沟矿区薄脉型铅锌银矿床地质特征及勘查实践经验总结.矿产勘查,待刊
刘荣绰,张泰华.1981.三道庄层状夕卡岩钼钨矿床的一般特征.河南地质,(1)：11-22
刘孝善,严正富,郑素娟,武耀成,黄标,吴澄宇.1987.东秦岭有色金属成矿带中典型矿床赋矿地层的地质地球化学研究.矿床地质,6(4)：1-10
刘孝善,孙晓明.1989.金堆城铝矿床成矿流体包裹体及稳定同位素研究.地质与勘探,25(2)：12-20
刘勇胜,袁洪林,高山,胡兆初,王选策,柳小明,凌文黎.2004.汉诺坝橄榄辉石岩包体锆石U-Pb年龄：97-158 Ma岩浆底侵作用和麻粒岩相变质作用之间的成因联系.科学通报,49(8)：790-797
娄德波,肖克炎,丁建华,孙艳.2010.矿产资源评价系统(MRAS)在全国矿产资源潜力评价中的应用.地质通报,29(11)：1677-1684.
卢欣祥,孔大刚.1982.河南省秦岭-大别山地区燕山期主要中酸性小岩体硫同位素组成特征.河南地质,1982(2)：7-12
卢欣祥.1983.河南省秦岭-大别山地区燕山期中酸性小岩体的基本地质特征及成矿专属性.河南地质,1(1)：49-55
卢欣祥.1988.龙王石童碱性花岗岩——东秦岭最大A型花岗岩的地质矿化特征及意义.见：张国伟等著.秦岭造山带的形成与其演化.西安：西北大学出版社,135-147
卢欣祥,董有,常秋岭,肖庆辉,李晓波,王晓霞.1996.秦岭印支期沙河湾奥长环斑花岗岩及其动力学意义.中国科学(D辑),26(30)：244-248
卢欣祥.1999.秦岭花岗岩大地构造图.西安：西安地图出版社
卢欣祥,于在平,冯有利,王义天,马维峰,崔海峰.2002.东秦岭深源浅成型花岗岩的成矿作用及地质构造背景.矿床地质,21(2)：168-178
卢欣祥,尉向东,董有,于在平,常秋玲,等.2004.小秦岭-熊耳山地区金矿特征与地幔流体.北京：地质出版社,102-119
陆松年,李怀坤,陈志宏,等.2003.秦岭中-新元古代地质演化及对Rodinia超级大陆事件的响应.北京：地质出版社,163-174
陆松年,陈志宏,李怀坤,郝国杰,周红英,相振群.2004.秦岭造山带中-新元古代(早 期)地质演化.地质通报,23(2)：107-112
栾世伟,陈尚迪,等.1991.小秦岭地区深部金矿化特征及评价.成都：成都科技大学出版社
罗铭玖.1981.河南斑岩钼矿矿化分带、矿床型式及成矿规律初探.河南地质,(1)：1-10
罗铭玖,董群英,李兴福,李昆华.1985.河南栾川南泥湖-三道庄钼钨矿床的地质特征及矿床类型.河南地质,3(增刊)：237-245
罗铭玖,张辅民,董群英,等.1991.中国钼矿床.郑州：河南科学技术出版社,118-408
罗铭玖,黎世美,卢欣祥,郑德琼,苏振邦.2000.河南省主要矿产的成矿作用及矿床成矿系列.北京：地质出版社,244-287
罗平,魏英文,王永庆.2005.北武夷长寿源银铅(锌)矿床地质特征.资源调查与环境,26(1)：33-42
吕庆田,侯增谦,赵金花,史大年,吴宣志,常印佛,裴荣富,黄东定,匡朝阳.2003.深地震反射剖面揭示的铜陵矿集区复杂地壳结构形态.中国科学(D辑),33(5)：442-449
吕庆田,侯增谦,杨竹森,史大年.2004.长江中下游地区的底侵作用及动力学演化模式：来自地球物理资料的约束.中国科学(D辑),34(9)：783-794
吕仁生.1987.三道庄钼钨矿床矿液流向的研究.河南地质,5(3)：14-18
吕文德,孙卫志,王喜恒,肖中军,徐文超,杨国强.2002.河南省栾川赤土店地区银铅锌成矿地质条件及找矿前景.前寒武纪研究进展,25(3-4)：165-169
吕文德,孙卫志.2004.卢氏-栾川地体铅锌矿成矿地质条件分析及找矿远景.矿产与地质,18(6)：507-516
吕文德,赵春和,孙卫志,燕建设.2005.河南栾川地区矽卡岩型铅锌矿地质特征——南泥湖钼矿外围找矿问题.地质调查与研究,28(1)：25-31
毛景文,王志良.2000.中国东部大规模成矿时限及其动力学背景的初步探讨.矿床地质,19(4)：289-296
毛景文,张作衡,余金杰,王义天,牛宝贵.2003.华北及邻区中生代大规模成矿的地球动力学背景：从金属矿床年龄精测得到启示.中国科学(D辑),33(4)：289-299
毛景文,李晓峰,张荣华,王义天,赫英,张作衡,等.2005.深部流体成矿系统.北京：中国大地出版社,5-11
毛景文,郑榕芬,叶会寿,高建京,陈文.2006.豫西熊耳山地区沙沟银铅锌矿床成矿的40Ar-39Ar年龄及其地质意义.矿床地质,25(4)：359-368
倪师军.1994.小秦岭中基性岩脉秘金矿成因关系新模式.西安：西安交通大学出版社,1-132
倪志耀,王仁民,童英,杨淳,戴潼谟.2003.河南洛宁太华岩群斜长角闪岩的锆石207Pb/206Pb和角闪石40Ar/39Ar年龄.地质论评,49(4)：361-366
倪智勇,李诺,管申进,张辉,薛良伟.2008河南小秦岭金矿田大湖金-钼矿床流体包裹体特征及矿床成因.岩石学报,24(9)：2058-2068
倪智勇,李诺,张辉,薛良伟.2009.河南大湖金钼矿床成矿物质来源的锶钕铅同位素约束.岩石学报,25(11)：2823-2832
裴荣富.1995.中国矿床模式.北京：地质出版社,1-120
裴先治,李厚民,李国光.1996.东秦岭商丹断裂带南侧变质基性岩的时代和岩石地球化学特征.西北地质科学,16(2)：49-57
裴先治.1997.东秦岭商丹构造带的组成与构造演化.西安：西安地图出版社,1-133
裴先治,王涛,王洋,李厚民,李国光.1999.北秦岭晋宁期主要地质事件及其构造背景探讨.高校地质学报,5(2)：137-147
彭恩生.1994.篙坪沟-铁炉坪地区银金多金属矿床成矿地质特征.中南矿冶学院学报,25(4)：427-430
彭万夫.1981.秦岭东段中酸性小岩体岩石化学成分的演化特征及与以钼为主的成矿关系.河南地质,(4)：1-13.
彭万夫.1986.秦岭-大别山区燕山期中酸性小岩体岩石化学成分及含矿性.河南地质,4(3)：1-13
齐金忠,马占荣,李莉.2004.河南祁雨沟金矿床成矿流体演化特征.黄金地质,10(4)：1-10
祁进平,宋要武,李双庆,陈福坤.2009.河南省栾川县西沟铅锌银矿床单矿物铷-锶同位素组成特征.岩石学报,25(11)：2843-2854
乔怀栋,刘长命,董有,彭万夫.1983.初步探讨东秦岭地区与小岩体有关矿床的成矿模式.河南地质,1(1)：25-34
任富根,李维明,李增慧,等.1996.熊耳山-崤山地区金矿成矿地质条件和找矿综合评价模型.北京：地质出版社,1-120
任富根,李惠民,殷艳杰,李双保,丁士应,陈志宏.2000.熊耳群火山岩系的上限年龄及其地质意义.前寒武纪研究进展,23(3)：140-146
任富根,殷艳杰,李双宝,赵嘉农.2001.熊耳裂陷印支期同位素地质年龄耦合性.矿物岩石地球化学通讯,20(4)：286-288
任富根,李惠民,殷艳杰,李双保,丁士应,陈志宏.2002.豫西地区熊耳群的地质年代学研究.前寒武纪研究进展,25(1)：41-47
陕西省地质矿产局,1989.陕西省区域地质志.北京：地质出版社,1-700
邵克忠,王宝德,吴新国,等.1992.祁雨沟地区爆发角砾岩型金矿成矿地质条件及找矿方向研究.河北地质学院学报,15(2)：105-194
盛中烈,罗铭玖,李良骏.1980.豫西斑岩钼矿带的基本地质特征及主要成矿控制因素.地质学报,54(4)：300-309
盛中烈,温明星,隋慎范.1984.东秦岭钼多金属成矿带内地层在成矿过程中的作用.河南地质,2(1)：23-28
施俊法,肖庆辉.2004.经验勘查与理论勘查的发展趋势.地质通报,23(8)：809-815
石铨曾,尉向东,李明立.1995.小秦岭变质核杂岩基本特征及与金的成矿作用.河南地质矿产与环境论文集,1-196
石铨曾,陶自强,庞继群,曲明绪.1996.华北板块南缘栾川群研究.华北地质矿产杂志,11(1)：51-59
石铨曾,尉向东,李明立,庞继群.2004.河南省东秦岭山脉北缘的推覆构造及伸展拆离构 造.地质出版社,1-202
隋颖慧,王海华,高秀丽,陈华勇,李震.2000.河南铁炉坪银矿成矿流体研究及其对碰撞造山成岩成矿与流体作用模式例证.中国科学(D辑),30(增刊)：82-90
孙敏,张立飞,吴家弘.1996.早元古代宽甸杂岩的成因：地球化学证据.地质学报,70(3)：207-222
孙枢,从柏林,李继亮.1981.豫、陕中、晚元古代沉积盆地.地质科学,(4)：314-322
孙枢,张国伟,陈志明.1985.华北断块区南部前寒武纪地质演化.冶金工业出版社,1-216
孙晓明,刘孝善.1987.金堆城钼矿区两类不同花岗岩的关系及其成因研究.地质找矿论丛,2(2)：34-44
孙晓明,任启江,杨荣勇,徐兆文,刘孝善.1998.金堆城超大型钼矿床水-岩δD-δ18O同位素交换体系理论模型及成矿流体来源.地质地球化学,26(2)：16-21
孙勇,卢欣祥,韩松,张国伟,杨司祥.1996.北秦岭早古生代二郎坪蛇绿岩片的组成和地球化学.中国科学(D辑),26(增刊)：49-55
宋国耀,张晓华,肖克炎.矿产资源潜力评价的理论和GIS技术[R]
宋国耀,张晓华,肖克炎.1999.矿产资源潜力评价的若干问题[J].中国地质,1999.
王非,朱日祥,李齐,贺怀宇,罗清华,卢欣祥,桑海清,王英兰.2004.秦岭造山带的差异隆升特征——花岗岩10Ar-39Ar年代学研究的证据.地学前缘,11(4)：445-459
王海华,陈衍景,高秀丽.2001.河南省康山金矿同位素地球化学及其对成岩成矿及流体作用模式的印证.矿床地质,20(2)：190-198.
王昊,徐刚,路坦,刘旭,瞿东旭.2007.河南省银洞沟银多金属矿床地质特征及成因分析.矿产与地质,21(4)：429-435
王家枢,曹新元.2009.对矿产勘查工作规律的初步分析和归纳.国土资源情报,7：6-12
王天聪.1985.雷门沟钼矿床地质特征.河南地质,3(增刊)：270-272
王义天,毛景文,卢欣祥.2001.嵩县祁雨沟金矿成矿时代的40Ar/39Ar年代学证据.地质论评,47(5)：551-555
王义天,毛景文,卢欣祥,叶安旺.2002a.河南小秦岭金矿区Q875脉中深部矿化蚀变岩的40Ar/39Ar年龄及其意义.科学通报,47(18)：1427-1431
王义天,毛景文.2002b.碰撞造山作用期后仲展体制下的成矿作用—以小秦岭金矿集中区为例.地质通报,21(8-9)：562-566
王义天,毛景文,叶安旺,叶会寿,李永峰,卢欣祥,李永革.2005.小秦岭地区中深部含金石英脉的同位素地球化学特征及其意义.矿床地质,24(3)：270-279
王跃峰.2000.栾川群大红口组火山岩研究初探.河南地质,18(3)：181-189
王志光,崔毫,徐孟罗,等.1997.华北地块南缘地质构造演化与成矿.北京：冶金工业出版社,1-296
王作勋等.1995.秦岭造山带显生宙构造迁移与陶湾群沉积变形.北京：地震出版社
王浩丞,孙宝生.2010.矿产资源潜力评价研究现状及发展方向展望.西部探矿工程,2010(10)：165-166
魏庆国,姚军明,赵太平,孙亚莉,李晶,原振雷,乔波.2009.东秦岭发现-1.9(a钼矿床 -河南龙门店钼矿床Re-Os定年.岩石学报,25(11)：2747-2751
温森坡.2008.嵩县店房火山角砾岩体西段金成矿潜力分析.黄金,29(12)：15-18
吴福元,孙德有.1999.中国东部中生代岩浆作用与岩石圈减薄.长春科技大学学报,29(4)：313-318
吴福元,孙德有,张广良,任向文.2000.论燕山运动的深部地球动力学本质.高校地质学报,6(3)：379-388
吴华,李华芹,莫新华,陈富文,路远发,梅玉萍,邓岗.2005.新疆哈密白石泉铜镍矿区基性-超基性岩的形成时代及其地质意义.地质学报,79(4)：498-502
吴良士,邹晓秋.1997.江西城门山铜矿铼-锇I司位素年龄研究.矿床地质,16(4)：376-381
肖克炎,张晓华,王四龙,等.2000.矿产资源GIS评价系统.北京：地质出版社,142
肖克炎,张晓华,李景朝.2007.全国重要矿产总量预测方法[J].地学前缘,2007,14(5)：20-26.
肖克炎,丁建华,刘锐.2005.美国“三步式”固体矿产资源潜力评价方法评述[J].地质论评,2006,52(6)：793-798.
徐国风.1985.论豫西银家沟钼-铜-硫铁矿矿床的矿质来源.河南地质,3(增刊)：266-270
徐启东,钟增球,周汉文,杨发城,唐学超.1998.豫西小秦岭金矿区的一组40Ar/39Ar定年数据.地质论评,44(3)：323-327
徐士进.1985.河南栾川上房沟细脉浸染钼矿床围岩蚀变与成矿作用的关系及其地球化学特征.河南地质,3(4)：33-42
徐文超,庞振山,周奇明,王喜恒,杨国强.2003.河南省栾川县南泥湖钼钨矿田外围银铅锌多金属成矿地质条件分析及找矿前景.矿产与地质,17(3)：198-202
徐兆文,杨荣勇,刘红樱,陆现彩,徐文艺,任启江.1998a.陕西金堆城斑岩钼矿床成矿流体研究.高校地质学报,4(4)：423-431
徐兆文,杨荣勇,陆现彩,任启江.1998b.金堆城斑岩钼矿床地质地球化学特征及成因.地质找矿论丛,13(4)：18-27
许永仁.1985.洛南-豫西斑岩钼矿带控岩控矿构造环境初步分析.河南地质,3(增刊)：135-139
许志琴,卢一伦,汤耀庆,M. Mattaure, Ph. Matte, J. Malavieille, P. Tapponnier, H. Maluski.1986.东秦岭造山带的变形特征及构造演化.地质学报,60(3)：237-247
薛良伟,原振雷,张荫树,强立志.1995.鲁山太华岩群Sm-Nd司位素年龄及其意义.地球化学,24(增刊)：92-97
严正富,杨正光,程海,杨浩,付成义,吴智慧.1986.雷门沟钼矿化花岗斑岩成因浅析.南京大学学报,22(3)：525-535
燕长海,刘国印,宋锋,张正伟.2002.河南马超营-独树一带银铅锌成矿地质条件及找矿前景.中国地质,29(3)：305-310
燕长海,刘国印,邓军.2003.豫西南铅锌银矿集区深部构造与成矿作用.地质调查与研究,26(4)：221-227
燕长海,宋要武,刘国印,邢矿.2004a.河南栾川杨树凹-百炉沟MVT铅锌矿带地质特征.地 质调查与研究,27(4)：249-254
燕长海,刘国印.2004b.豫西南铅锌多金属矿控矿条件及找矿方向.地质通报,23(11)：1143-1148
燕长海.2004c.东秦岭铅锌银成矿系统内部结构.北京：地质出版社,46-96
杨进朝,冯胜斌,彭翼,燕长海,曾宪友,王建明,胡绍斌.2008.豫西嵩县上庄坪铅锌银矿床地球化学特征及地质意义.中国地质,35(02)：305-309
杨经绥,许志琴,斐先治,史仁灯,吴才来,张建新,李海兵,孟繁聪,戎合.2002.秦岭发现金刚石横贯中国中部巨型超高压变质带新证据及古生代和中生代两期深俯冲作用的识别.地质学报,76(4)：484-495
杨忆.1983.熊耳群钾质细碧-石英角斑岩岩石特征及成因探讨.1981届硕士学位论文集.北京：科学出版社
杨忆.1990.华北地台南缘熊耳群火山岩特点及形成的构造背景.岩石学报,(2)21-28
杨正光,严正富.1985.雷门沟钼矿化花岗斑岩特征及其成因系列的探讨.河南地质,3(增刊)：273-278
姚瑞增.1986.洛南.豫西斑岩钼矿带成岩成矿构造作用浅析.河南地质,4(4)：14-19
叶天竺.2012.固体矿产找矿预测方法研究纲要.内部资料
叶会寿,毛景文,李永峰,燕长海,郭保健,赵财胜,何春芬,郑榕芬,陈莉.2006a.豫西南泥湖矿田钼钨及铅锌银矿床地质特征及其成矿机理探讨.现代地质,20(1)：165-174
叶会寿,毛景文,李永峰,郭保健,张长青,刘珺,闫全人,刘国印.2006b.东秦岭东沟斑岩SHRIMP锆石U-Pb年龄和钼矿Re-Os年龄及其地质意义.地质学报,80(5)：1078-1088
叶玉丰.2004.基于GIS技术的矿产资源规划管理信息系统[J].地质与资源,2004,13(1)52-64.
袁学诚,徐明才,唐文榜等.1994.东秦岭陆壳反射地震剖面.地球物理学报,37(6)：749-758
袁跃清,王秀全,冯昂.2005.河南省西部四道沟银-铅矿区地质特征及找矿远景分析.矿产与地质,19(4)：371-374
曾华杰,张泰华,张炳欣,宋北城.1983.南泥湖钼矿田同熔型花岗岩类的成因研究.河南地质,1(1)：56-66.
曾华杰,张炳欣.1985.河南栾川南泥湖钼矿田矿床地质特征及其成因探讨.河南地质,3(增刊)：46-250
翟明国.2010.华北克拉通的形成演化与成矿作用.矿床地质,29(1)：24-36
翟裕生.1999.论成矿系统.地学前缘,6(1)：13-26
张本仁,骆庭川,高山,欧阳建平,陈德兴,马振东,韩吟文,谷晓明,等.1994.秦巴岩石圈构造及成矿规律地球化学研究.武汉：中国地质大学出版社,257-364
张本仁,张宏飞,赵志丹,凌文黎.1996.东秦岭及邻区壳、幔地球化学分区和演化及其大地构造意义.中国科学(D辑),26(3)：201-208
张本仁,高山,张宏飞,韩吟文,等.2002.秦岭造山带地球化学.北京：科学出版社,1-173
张德会.1997.成矿流体中金的沉淀机理研究述评.矿物岩石,17(4)：122-130
张国伟,孟庆任,于在平,孙勇,周鼎武,郭安林.1996.秦岭造山带的造山过程及其动力学特征.中国科学(D辑),26(3)：193-200
张国伟,张本仁,袁学诚,肖庆辉,等.2001.秦岭造山带与大陆动力学.北京：科学出版社,1-806
张进江,郑亚东,刘树文.1998.小秦岭变质核杂岩的构造特征、形成机制及构造演化.北京：海洋出版社,17-63.
张洪岩,王软敏,周成虎,等.2001.“数字地球”与地理信息科学[J].地球信息科
学,2001(4)：124.
张理刚.1989.成岩成矿理论与找矿—中国主要类型矿床及花岗岩类的稳定同位素地质学.北京：北京科技大学出版社,143
张理刚,刘敬秀,王可法,等.1995.东亚岩石圈块体地质-上地幔、基底和花岗岩同位素地球化学及其动力学.北京：科学出版社
张连昌,沈远超,李厚民,曾庆栋,李光明,刘铁兵.2002.胶东地区金矿床流体包裹体的He、Ar同位素组成及成矿流体来源示踪.岩石学报,18(4)：559-565
张乃昌,阎景汉,刘新年.1986.从重磁成果探讨我省深部构造及成矿作用.河南地质,4(1)：16-22.
张旗,张宗清,孙勇,韩松.1995.陕西商县-丹凤地区丹凤群变质玄武岩的微量元素和同位素地球化学.岩石学报,11(1)：43-54
张天义,王俊卿.1996.熊耳山、外方山地区金矿成矿条件的遥感地质特征.关保德著,河南华北地台南缘前寒武世地质和成矿,118-133。
张天义,朱嘉伟,盛吉虎.1997.秦岭大地构造格局的遥感地质分析.河南地质,15(3)：179-185
张瑜麟.2001.熊耳山银铅成矿区物探找矿方法应用研究.地质与勘探,37(6)：46-50
张瑜麟.2003.熊耳山西段银铅矿找矿地球物理标志研究.矿产与地质,2003
张正伟,朱炳泉,常向阳.2000.东秦岭北部富碱侵入岩钕、锶、铅同位素特征及构造意义.地球化学,29(5)：455-461
张正伟,邓军.2001.东秦岭钼矿带成矿背景与含矿岩体特征.陈衍景,张静,赖勇主编.大陆动力学与成矿作用.北京：地震出版社,100-109
张正伟,朱炳泉,常向阳.2003.东秦岭北部富碱侵入岩带岩石地球化学特征及构造意义.地学前缘,10(4)：507-519
张宗清,刘敦一,付国民.1994.北秦岭变质地层同位素年代研究.北京：地质出版社,1-200
张宗清,张国伟,唐索寒,广欣祥.1999.秦岭沙河湾奥长环斑花岗岩的年龄及其对秦岭造山带主造山期结束时问的限制.科学通报,44(9)：981-984
张宗清,张国伟,唐索寒.2002.南秦岭变质地层同位素年代学.北京：地质出版社,1-123
赵书梅.2008.多种地质找矿手段的综合应用.硅谷,19：4
赵太平,庄建敏,原振雷.1996.华北板块南缘熊耳群火山岩岩石类型及火山岩系列.华北地质矿产杂志,11(4)：599-606
赵太平,周美夫,金成伟,关鸿,李惠民.2001.华北陆块南缘熊耳群形成时代讨论.地质科学,36(3)：326-334
赵太平,金成伟,翟明国,夏斌,周美夫.2002.华北陆块南部熊耳群火山岩的地球化学特征与成因.岩石学报,18(1)：59-69
赵太平,翟明国,夏斌,李惠民,张毅星,万渝生.2004.熊耳群火山岩锆石SHRIMP年代学研究：对华北克拉通盖层发育初始时间的制约.科学通报,49(22)：2342-2349
赵振华,涂光炽.2003.中国超大型矿床(Ⅱ).北京：科学出版社,523-542
郑建平,路凤香,郭晖,任迎新.1994.金刚石中流体包裹体的研究.科学通报,39(3)：253-256
郑榕芬,毛景文,高建京.2004.河南熊耳山沙沟银铅锌矿床中硫化物和银矿物的矿物学特征及其意义.矿床地质,25(6)：715-726
支风岐,刘灵恩,索勇.2004.河南省熊耳山西段沙沟西银铅矿区地质特征及找矿前景分析.矿产与地质,18(1)：35-38
周珂,叶会寿,毛景文,屈文俊,周树峰,孟芳,高亚龙.2009.豫西鱼池岭斑岩型钼矿床地质特征及其辉钼矿铼-锇同位素年龄.矿床地质,28(2)：170-184
朱炳泉.1993.矿石铅同位素三维拓扑图解用于地球化学省与矿种区划.地球化学,22(3)：209-216
朱炳泉.1998.壳幔化学不均一性与块体地球化学边界研究.地学前缘,5(1-2)：72-82
朱嘉伟,张天义,薛良伟.1999.豫西崤山地区金矿成矿年龄的测定及其意义.地质论评,45(4)：418-422
朱裕生,王柏钧.矿产资源评价的现状和展望[R]
BartosPJ.1987. Quiruvilca, Peru:Mineral zoning and timing of wall-rock alteration relative to Cu-Pb-Zn-Ag vein-fill deposition. Economic Geology,82:1431-1452.
Bendezu R and Pontbote 1..2002. Late timing for high-sulf idation Cordilleran base metal lode and replacement deposits in porphyry-related districts:the case of Colquijirca, central Peru. Society for Geology Applied to Mineral (SGA) News 13,9-13.
Bendezu R, Page L, Spikings R, Pecskay Z, Fontbote L.2008. New 40Ar/39Ar alunite ages from the Colqui jirca district, Peru:evidence of a long period of magmatic SO2 degassing during formation of epi thermal Au-Ag and Cordilleran polymetallic ores. Mineralium Deposita,43(7):777-789.
Bendezu R and Fontbote L. 2009. Cordilleran Epithermal Cu-Zn-Pb-(Au-Ag) Mineralization in the Colquijirca District, Central Peru:Deposit-Scale Mineralogical Patterns. Economic Geology,104(7):905-944
Bonham-Cater GF.1994. Geographic information systems for geoscientists:modelling with GIS. Oxford:Pergamon Press,398.
Boorder H, Spakman W, White SHetal.1998. Late Cenozoic mineralization, orogenic collapse and slab detachment in the European Alpine Belt. Earth and Planetary Science Letters.,164:569-575
Bouabdellah M, BeaudoinG, Leach DL.2009. Genesis of the Assif El Mal Zn-Pb(Cu, Ag)vein deposit. An extension-related Mesozoic vein system in the High Atlas of Morocco. Structural, mineralogical, and geochemical evidence. Mineralium Deposita,44(6):689-704
Cabri LJ.1987. The mineralogy of precious metals:new developments and metallurgical implications. Canadian Mineralogist,25(1):1-7
Cabri LJ.1992. The distribution of trace precious metals in minerals and mineral products. Mineralogical Magazine,56(3):289-308
Chen YJ, Pirajno F and Sui YH.2004. Isotope geochemistry of the Tieluping silver deposit, Henan, China:A case study of orogenic silver deposits and related tectonic setting. Mineral ium Deposita.39:560-575
Chen YJ, Franco P and Sui YH.2005. Geology and D-O-C isotope systematics of the Tieluping silver deposit, Henan, China:Implications for Ore Genesis. Acta Geologica Sinica,79(1):106-119
Chen YJ, Pirajno F, Qi JP.2008. The Shanggong gold deposit. Eastern Qinl ing Orogen, China:Isotope geochemistry and implications for ore genesis. Journal of Asian Earth Sciences,33(3-4):252-266
Cheng Guang-guo, Feng You-li, Yu Li-jing.2011. The application of GIS in management of mineral resources,20112nd International Conference on Artificial Intelligence, Management Science and Electronic Commerce,9:7317-7319
Costagliola P, Di Benedetto F, Banvenuti M, Bernardini GP, Cipriani C, Lattanzi PF, Romanelli M.2003. Chemical speciation of Ag in galena by EPR spectroscopy. American Mineralogist,88(8-9):1345-1350
Cox DP and Singer MA.1986. Mineral deposits models. U.S. Geological Survey Bulletin 1693:1-379
Creaser RA, Papanastassiou DA and Wasserburg GJ.1991. Negative thermal ion mass spectrometry of osmium, rhenium, and iridium. Geochim. Cosmochim. Acta.,55: 397-401
Einaudi MT.1982. General features and origin of skarns associated with porphyry copper plutons,In:Titley SR(ed.), Advance in geology of the porphyry copper deposits, Southwestern North America, University of Arizona Press, Tuscon, 185-209
Fan HR and Xie YH.1999. Porphyry-type molybdenum deposits in the eastern Qinling Mo belt, central China. Scientia Geologica Sinica,8(1):91-101
Foord EE, Shawe DR.1989. The Pb-Bi-Ag-Cu-(Hg)chemistry of galena and some associated sulfosalts:a review and some new data from Colorado, California and Pennsylvania. Canadian Mineralogist.27(3):363-382.
Gammons CH, Barnes HL.1989. The solubility of Ag2S in near-neutral aqueous sulf ide solutions at25 to 300 "C. Geochimica et Cosmochimica Acta,53(2):279-290
GaoS, Zhang BR, Jin ZM, Kern H, Luo TC and Zhao ZD.1998. How mafic is the lower continental crust? Earth and Planetary Science Letters,106:101-117
Gasparrini C.1984. The Mineralogy of Silver and Its Significance in Metal Extraction. Canadian Mining and Metallurgical Bulletin,77(866):99-110
Gasparrini C, Lowell GR.1985. Silver-bearing inclusions in "argentiferous" galena from the Silvermine district in southeastern Missouri. Canadian Mineralogist, 23(1):99-102
Gilbert JM and Park JR.1986. The geology of ore deposits. New York:Freeman and Co.,750
Giordano TH, Barnes HL.1979. Ore solution chemistry VI. PbS solubility in bisulfide solutions to 300℃. Economic Geology,74(7):1637-1646
Han YG, Zhang SH, Pirajno F, Wang Y, Zhang YH.2009. New 40Ar-39Ar age constraints on the deformation along the Machaoying fault zone:Implications for Early Cambrian tectonism in the North China Craton. Gondwana Research,16(2):255-263
Hayashi K, Sugaki A, Kitakaze A.1990. Solubility of sphalerite in aqueous sulfide solutions at temperatures between25 and240℃. Geochimica et Cosmochimica Acta, 54(3):715-725
He YH, Zhao GC, Sun M, Wilde SA.2008. Geochemistry, isotope systematics and petrogenesis of the volcanic rocks in the Zhongtiao Mountain:An alternative interpretation for the evolution of the southern margin of the North China Craton. Lithos,102(1-2):158-178
He YH, Zhao GC, Sun M, Han YG.2010. Petrogenesis and tectonic setting of volcanic rocks in the Xiaoshan and Waifangshan areas along the southern margin of the North China Craton:Constraints from bulk-rock geochemistry and Sr-Nd isotopic composition. Lithos,114(1-2):186-199
He YH, Zhao GC, Sun M, Xia Xiaoping.2009. SHRIMP and LA-ICP-MS zircon geochronology of the Xiong'er volcanic rocks:Implications for the Paleo-Mesoproterozoic evolution of the southern margin of the North China Craton. Precambrian Research,168(3-4):213-222.
Hedenquist JW, Arribas A, Reynolds TJ.1998. Evolution of an intrusion-centered hydrothermal system; Far Southeast-Lepanto porphyry and epithermal Cu-Au deposits, Philippines. Economic Geology,93(4):373-404
Hemley JJ and Hunt JP.1992. Hydrothermal ore-forming processes in the light of studies in rock-buffered systems:Ⅱ. Some general geologic applications. Economic Geology,87:23-43.
Henley RW and Ellis AJ.1983. Geothermal systems, ancient and modern. Earth Science Reviews,19:1-50
Hu HB, Mao JW, Liu DY, Niu SY, Wang YB, Li YF and Shi RR.2005. SHRIMP Zircon U-Pb Dating of the Tongshi Magmatic Complex in Western Shandong and Its Geological Implications. Acta Geologica Sinica,79(4):491-496
Jiang N, Xu JH, Song MX.1999. Fluid inclusion characteristics of mesothermal gold deposits in the Xiaoqinling district, Shaanxi and Henan Provinces, People's Republic of China. Mineralium Deposita,34(2):150-162
Kroner A, Composton W, Zhang GW, Guo AL, Todt W.1988. Age and tectonic setting of Late Archean greenstone-gneiss terrain in Henan Province, China, as revealed by single-grain zircon dating. Geology,16:211-215
Kusky TM, Windley BF, Zhai MG.2007. Tectonic evolution of the North China Block: from orogen to craton to orogen. Geolocial Society of London Special Publications,280:1-34
Li YF, Mao JW, Guo BJ, Shao YJ, Fei HC and Hu HB.2004. Re-Os isotopic dating of molybdenites in the Nannihu Mo (W) ore field in the east Qinling and Its Geodynamic processes. Acta Geologica Sinica,78(2):463-470
Leach DL, Bradley D, Lewchuk MT, Symons DT, de Marsily G, Brannon J.2001. Mississippi Valley-type lead-zinc deposits through geological time: implications from recent age-dating research. Mineralium Deposita,36(8): 711-740
Leach TM and Corbett GJ.1993. Porphyry-related carbonate-base metal gold systems: The transition between the epithermal and porphyry environments. In Second National Meeting Specialist Group in Economic Geology, Armidale, N. S.W., Geological Society of Australia Abstracts,34:39-40
Leach TM and Corbett GJ.1994. Porphyry-related carbonate-base-metal gold systems in the southwest Pacific:characteristics. In:Rogerson R(ed.), Geology, exploration and mining conference proceedings, Parkville, The Australasian Institute of Mining and Metallurgy,84-91
Lu SN, Zhao GC, Wang HC, Hao GJ.2008. Precambrian metamorphic basement and sedimentary cover of the North China Craton:A review. Precambrian Research, 160(1-2):77-93
Lueth VW, Megaw PKM, Pingitore NE.2000. Systematic variation in galena solid-solution compositions at Santa Eulalia, Chihuahua, Mexico. Economic Geology,95(8):1673-1678
Macfarlane AW and Petersen U.1990. Pb isotopes of the Hualgayoc area, northern Peru:Implications for metal provenance and genesis of a Cordilleran polymetallic mining district. Economic Geology,85:1303-1327.
Mao JW, Kerrich R, Li HY and Li YH.2002a. High Wife ratios in the Wangu gold deposit, Hunan Province, China:implications for mantle fluid along the Tanlu deep fault zone. Geochemical Journal,36(3):197-208
Mao JW, Wang YT, Ding TP, Chen YC, Wei JX and Yin JZ.2002b. Dashuigou Tellurium Deposit in Sichuan Province, China-An Example of Mantle Fluid Evolving in Mineralized Process:Evidences from C,0, H, S Isotopes. Resource Geology, 52(1):15-23
Mao JW, Goldfarb RJ, Zhang ZW, Xu WY, Qiu YM and Deng J.2002. Gold deposits in the Xiaoqinling-Xiong'ershan region. Qinling Mountains, central China. Mineralium Deposita,37:306-325
Mao JW, Li YQ, Goldfrab R, He Y and Zaw K.2003. Fluid inclusions noble gas studies of the Dongping gold deposit, Heibei Province, China:A mantle connection for mineralization. Economic Geology,98:517-534
Mao JW, Wang YT, Zhang ZH, Yu JJ, Niu BG.2003. Geodynamic settings of Mesozoic large-scale mineralization in North China and adjacent areas—Implication from the highly precise and accurate ages of metal deposits. Science in China (Series D),46(8):838-851
Mao JW, Xie GQ, Bierlein F, Qu WJ, Du AD, Ye HS, Pirajno F, Li HM, Guo BJ, Li YF, Yang ZQ.2008. Tectonic implications from Re-Os dating of Mesozoic molybdenum deposits in the East Qinling-Dabie orogenic belt. Geochimica et Cosmochimica Acta,72(18):4607-4626.
Merrihue C and turner G.1962. Potassium-argon dating by activation with fast neutrons. J. Geophys. Res,71:2852-2857
Mitchell AHG and Garson MS.1981. Mineral deposits and global tectonic settings. London:Academic Press,1-457
Pearce JA, Lippard SJ and Roberts S.1984. chteristics and tectonic significance of supra-subduction zone ophiolites. Marginal Basin Geology,16 (Geol Soc Spec Pub 1):77-93
Peng P, Zhai MG, Guo JH, Kusky T, Zhao TP.2007. Nature of mantle source contributions and crystal differentiation in the petrogenesis of the 1.78 Ga mafic dykes in the central North China craton. Gondwana Research,12(1-2):29-46
Peng P, Zhai MG, Ernst RE, Guo JH, Liu F, Hu B.2008. A 1.78 Ga large igneous province in the North China craton:The Xiong'er Volcanic Province and the North China dyke swarm. Lithos,101 (3-4):260-280
Ratschbacher L, Hacker BR, Andrew Calvert A, Webb LE, Grimmer JC, McWilliams MO, Ireland T, Dong SW and Hu JM.2003. Tectonics of the Qinl ing (Central China): tectonostratigraphy, geochronology, and deformation history. Tectonopysics, 366(1-2):1-53
Ruaya JR, Seward TM.1986. The stability of chlorozinc (Ⅱ)complexes in hydrothermal solutions up to 350℃. Geochimica et Cosmochimica Acta,50(5):651-661
Sawkins FJ.1984. Metal deposits in relation to plate tectonics. Springer-Verlag, Berlin, Heidelberg, New York, Tokyo,1-325
SawkinsFJ.1990. Metal Deposits in Relation to Plate Tectonics (2nd edition). Berlin: Springer-Verlag,1-461
Seward TM.1976. The stability of chloride complexes of silver in hydrothermal solutions up to 350℃. Geochimica et Cosmochimica Acta,40(11):1329-1341
Seward TM.1984. The formation of lead(Ⅱ)chloride complexes to 300℃:a spectrophotometric study. Geochimica et Cosmochimica Acta,48(1):121-134
Sharp TG and Buseck PR.1993. The distribution of Ag and Sb in galena:inclusions versus solid solution. American Mineralogist,78(1-2):85-95
Shirey SB and Walker RJ.1995. Carius tube digestion for low-blank rhenium-osmium analysis. Anal. Chem.,67:2136-2141
Stefansson, A. Seward, T. M.2003. Experimental determination of the stability and stoichiometry of sulphide complexes of silver(Ⅰ)in hydrothermal solutions to 400 ℃. Geochimica et Cosmochimica Acta,67(7):1395-1413
Stein HJ, Markey RJ, Morgan JW, Du A and Sun Y.1997. Highly precise and accurate Re-Os ages for molybdenite from the East Qinling molybdenum belt, Shanxi Province, China. Economic Geolology,92:827-835.
Sun X, Gong QJ, Wang QF, Yang LQ, Wang CM, Wang ZL.2010. Application of local singularity model to delineate geochemical anomalies in Xiong'ershan gold and molybdenum ore district, We stern Henan province, China. Journal of Geochemical Exploration,107(1):21-29
Suzuki K, Lu Q, Shimizu H, et al.1993. Reliable Re-Os age for molybdenite. Geochim. Cosmochim. Acta,57:1625-1628
Taylor SR and Mclennan SM.1985. The Continental Crust:its Composition and Evolution. BlackwelllScientific Publications, Oxford,312
Voudouris P, Melfos V, Spry PG.2008. Carbonate-replacement Pb-Zn-Ag ± Au mineralization in the Karnariza area, Lavrion, Greece:mineralogy and thermochemical conditions of formation. Mineralogy and Petrology,94(1-2): 85-106
Wan YS, Song B, Liu DY, Wilde SA, Wu JS, Yin XY, Zhou HY.2006. SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary rocks in the North China Craton:Evidence for a major Late Palaeoproterozoic tectonothermal event. Precambrian Research,149(3-4):249-271
Wang XL, Jiang SY, Dai BZ.2010. Melting of enriched Archean subcontinental lithospheric mantle:Evidence from the ca.1760 Ma volcanic rocks of the Xiong'er Group, southern margin of the North China Craton. Precambrian Research,182(3):204-216
Wilson JT, Static and mobile earth:The current scientific revolution in the earth. Proc. Am Phil. Soc.1968,112:309-320
Wyborn LAI, Valenta PK, Jagodzinski EA, Morse M, Wellman P.1989. Integration of Multiple geoscience data sets in the Coronation Hill region, NT, as an aid to delineate areas of potential mineralisation. BMR Research Symposium 1989.
Yang JH, Wu FY, Wilde SA.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
Zeng NS, Izawa E, Motomura Y, Lai LR.2000. Silver minerals and paragenesis in the Kangjiawan Pb-Zn-AgAu deposit of the Shuikoushan mineral district, Hunan Province, China.Canadian Mineralogist,38(1):11-22
Zhai MG, Liu WJ.2003. Palaeoproterozoic tectonic history of the North China craton: a review. Precambrian Research,122(1-4):183-199
Zhang DH, Xu GJ, Zhang WH, Golding SD.2007. High salinity fluid inclusions in the Yinshan polymetallic deposit from the Le-De metallogenic belt in Jiangxi Province, China:Their origin and implications for ore genesis. Ore Geology Reviews,31:247-260
Zhang SH, Li ZX, Wu HC.2006. New Precambrian palaeomagnetic constraints on the position of the North China Block in Rodinia. Precambrian Research, 144(3-4):213-238
Zhao GC, Sun M, Wilde SA, Li SZ.2003. Assembly, Accretion and Breakup of the Paleo-Mesoproterozoic Columbia Supercontinent:Records in the North China Craton. Gondwana Research,6(3):417-434
Zhao GC, Sun M, Wilde SA, Li SZ.2004. A Paleo-Mesoproterozoic supercontinent: assembly, growth and breakup. Earth-Science Reviews,67(1-2):91-123
Zhao GC, He YH, Sun M.2009. The Xiong'er volcanic belt at the southern margin of the North China Craton:Petrographic and geochemical evidence for its outboard position in the Paleo-Mesoproterozoic Columbia Supercontinent. Gondwana Research,16(2):170-181.
Zhao TP, Zhou MF.2009. Geochemical constraints on the tectonic setting of Paleoproterozoic A-type granites in the southern margin of the North China Craton. Journal of Asian Earth Sciences,36(2-3):183-195
Zhou TH, Goldfarb RJ, Phillips NG.2002. Tectonics and distribution of gold deposits in China-an overview. Minealimu Deposita,37(3-4):249-282
白凤军,赵太平,肖荣阁,刘国营.2010.河南嵩县钾长石石英脉型钼矿成矿流体地球化学.现代地质,24(1)：26-33
白瑾,戴风岩,颜耀阳.1997.中条山前寒武纪地壳演化.地学前缘,4(3-4)：281-289
包志伟,李创举,祁进平.2009.东秦岭铅锌银矿田辉长岩钻石SHRIMP铀-铅年龄及成矿时代.岩石学报,24(11)：2951-2956
曹荣,龙朱华寿.1995.地幔流体与成矿作用.地球科学进展,10(4)：324-329
曹烨,李胜荣,申俊峰,要梅娟,李庆康,毛付龙.2008.豫西前河构造蚀变岩型金矿成矿过程中的流体-岩石反应.矿床地质,27(6)：714-726
曹烨,李胜荣,申俊峰,要梅娟.2009.豫西前河金矿热液蚀变地球化学研究.中国地质,(1)：
陈江峰,谢智,刘顺生,李学明,K. A. Folan.1995.大别造山带冷却年龄的40Ar-39Ar和裂变径迹年龄测定.中国科学(B辑),25(10)：1086-1092
陈书中,狄卫民.2002.干树金矿V-#脉地质特征及成矿预测探讨.金属矿山,(4)：58-60
陈旺,郭时然.1994.河南洛宁蒿坪沟银铅金矿床地质特征.有色金属矿产与勘查,3(6)：336-341
陈旺.1995.豫西熊耳山金矿床和银(铅)矿床铅同位素研究.贵金属地质,4(3)：168-176
陈旺,郭时然,崔毫.1996.豫西熊耳山铁炉坪、蒿坪沟矿床银铅矿石稳定同位素研究.有色金属矿产与勘查,4(4)：213-218
陈伟军,刘红涛,张德会.2007.河北丰宁牛圈银矿床流体包裹体特征及地质意义.矿产与地质,21(1)：12-16
陈衍景,富士谷.1992.豫西金矿成矿规律.北京：地震出版社,1-188
陈衍景,隋颖慧,Franco PIRAJNO.2003.CMF模式的排他性依据和造山型银矿实例东秦岭铁炉坪银矿同位素地球化学.岩石学报,19(3)：551-568
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
陈毓川,朱裕生.1991.中国矿床成矿模式.北京：地质出版社,1-367
陈毓川.1994.矿床的成矿系列.地学前缘,1(4)：90-94
陈毓川,薛春纪,王登红,李华芹,路远发.2003.华北陆块北缘区域矿床成矿谱系探讨.高校地质学报,9(4)：520-535
程裕淇,陈毓川,赵一鸣.1979.初论矿床的成矿系列问题.中国地质科学院院报,第1号,1-55
程广国.1994.河南熊耳山地区中生代花岗岩成因及构造环境与成矿关系,有色金属矿产与勘查,1994(1)
程广国.1997.河南瑶沟金矿矿床地球化学特征及成矿预测模型模型,有色金属矿产与勘查,1997(2)
陈郑辉,陈毓川,王登红,等.2009.矿产资源潜力评价示范研究—以南岭东段钨矿资源潜力评价为例
戴宝章,蒋少涌,王孝磊.2009.河南东沟铝矿花岗斑岩成因：岩石地球化学、锆石U-Pb年代学及Sr-Nd-Hf同位素制约.岩石学报,25(11)：2889-2901
邓晋福,赵海玲,莫宣学.1996.中国大陆根-柱构造：大陆动力学的钥匙.北京：地质出版社,1-110
邓小华,陈衍景,姚军明,李文博,李诺,王运,糜梅,张颖.2008a.河南省洛宁县寨凹钼矿床流体包裹体研究及矿床成因.中国地质,35(6)：1250-1266
邓小华,李文博,李诺,糜梅,张颖.2008b.河南嵩县纸房钼矿床流体包裹体研究及矿床成因.岩石学报,24(9)：2133-2148
邓小华,姚军明,李晶.2009.东秦岭寨凹钼矿床辉钼矿Re-Os同位素年龄及熊耳期成矿事件.岩石学报,25(11)：2739-2746
邓亚婷,王北颖.1988.小秦岭小河岩体岩石谱系单位划分及其定位机制.陕西地质,16(2)：2-7
董有,彭万夫,乔怀栋,刘长命,冯祖钧,武跃诚.1983.豫西—洛南中酸性小岩体成钼地质条件的定量分析与统计预测模型.河南地质,1(2)：62-74
董有.1986.豫西—洛南斑岩铝矿带成岩成矿几个问题的探讨.河南地质,4(3)：14-20
杜安道,何红蓼,殷宁万,等.1994.辉钼矿的铼-锇同位素地质年龄测定方法研究.地质学报,68(4)：339-347
杜安道,赵敦敏,王淑贤,孙德忠,刘敦一.2001.Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄.岩矿测试,20(4)：247-252
杜乐天.1986b.碱交代作用的地球化学原理.中国科学(B),81-90
杜乐天.1988.幔汁H-A-C-O-N-S流体.大地构造与成矿学,12(1)：87-94
杜乐天.1989.幔汁(HACONS流体)的重大意义.大地构造与成矿学,13(1)：91-99
杜乐天.1990.幔汁(HACONS)假说.矿物岩石地球化学通讯,(1)：39-42
杜乐天.1996a.地壳流体与地幔流体问的关系.地学前缘,172-180
范宏瑞,谢奕汉,王英兰,赵瑞.1994.康山金矿地质地球化学特征及其成因.黄金,15(3)：1-6
范宏瑞,谢奕汉,郑学正,王英兰.2000.河南祁雨沟热液角砾岩体型金矿床成矿流体研究.岩石学报,16(4)：559-563
冯守忠,冯淼.2000.吉林山门银金矿床地质特征.贵金属地质,9(1)：15-19
高建京,毛景文,叶会寿,陈懋弘,郑榕芬.2010.豫西沙沟脉状Ag-Pb-Zn矿床地质特征和成矿流体研究.岩石学报,26(3)：740-756
高山,张本仁,金振民.1999.秦岭-大别造山带下地壳拆沉作用.中国科学,29(6)：532-541
耿元生,杨崇辉,宋彪,万渝生.2004.吕梁地区18亿年的后造山花岗岩：同位素年代和地球化学制约.高校地质学报,10(4)：477-487
贡二辰.2008.河南省洛宁县蒿坪沟银金多金属矿区地质特征及找矿方向分析.地质与勘探,44(1)：21-25
关保德,吕国芳,王耀霞.1993.河南省地台区中-晚元古代构造沉积盆地演化分析.河南地质,11(3)：181-190
郭保健,徐孟罗,王志光,戴塔根.1997.熊耳山北坡拆离断层带地球化学特征及其与金银矿化的关系.矿产与地质,11(1)：20-25
郭保健,李永峰,王志光,叶会寿.2005.熊耳山Au-Ag-Pb-Mo矿集区成矿模式与找矿方向.地质与勘探,41(5)：43-47
郭东升,陈衍景,祁进平.2007.河南祁雨沟金矿同位素地球化学和矿床成因分析.地质论评,53(2)：217-227
郭力宇,王树洗,赵东宏,陈有仓.1997.陕西洛南陶湾群三岔口组砾岩研究.地球学报,18(4)：352-357
郭奇斌.1992.从地球物理场特征谈河南地质构造.河南地质,10(4)：264-272
郭时然.1995.洛宁铁炉坪银铅矿床围岩蚀变分带特征.河南地质,13(1)：9-14
韩以贵,李向辉,张吐红,张元厚,陈福坤.2007.豫西祁雨沟金矿单颗粒和碎裂状黄铁矿Rb-Sr等时线定年.科学通报,52(11)：1307-1311
何红蓼,杜安道,邹晓秋,等.1993.铼-锇同位素的等离了体质谱测定及其在辉钼矿测年中的应用.岩矿测试,12(3)：161-165.
河南省地质矿产局.1989.河南省区域地质志.北京：地质出版社,1-722
何云龙,魏俊浩,谭文娟,李晶.2008.山西堡子湾隐爆角砾岩型金矿矿床隐爆机制研究.矿产与地质,22(5)：377-380
胡受奚,林潜龙,陈泽铭,等.1988.华北与华南古板块拼合带地质和成矿.南京：南京大学出版社,1-558
胡文瑄,孙睿,张文兰.2001.金矿成矿流体的特点及深-浅部流体相互作用成矿机制.地学前缘,8(4)：281-288
胡正国,钱壮志,阎广民,陈在劳,李民贤.1994.小秦岭拆离-变质核杂岩构造与金矿.西 安：陕西科学出版社,1-200
胡志宏,周顺之,胡受奚,陈泽铭.1986.豫西太华岩群混合岩特征及其与金钼矿化的关系.矿床地质,5(4)：71-81
胡志宏,胡受奚,周顺之.1990.东秦岭燕山期大陆内部挤压-俯冲背景的A型孪生花岗岩带.岩石学报,(1)：1-12
华仁民,陈培荣,张文兰,姚军明,林锦富,张展适,顾晟彦.2005.南岭与中生代花岗岩类有关的成矿作用及其大地构造背景.高校地质学报,11(3)：291-304
黄楚秀,黄建军.1985.小秦岭地区中生代花岗岩类成因系列及其与成矿关系.河南地质,3(增刊)：123-128
黄典豪,王义昌,聂凤军,江秀杰.1984.黄龙铺碳酸盐脉型钼(铅)矿矿床的硫、碳、氧同位素组成及成矿物质来源.地质学报,58(3)：252-264
黄典豪,王义昌,聂凤军,江秀杰.1985.一种新的钼矿床类型—陕西黄龙铺碳酸盐脉型钼(铅)矿矿床地质特征及成矿机制.地质学报,59(3)：241-257
黄典豪,吴澄宇,聂凤军.1987.陕西金堆城斑岩钼矿床地质特征及成因探讨.矿床地质,6(3)：22-34
黄典豪,董群英,甘志贤.1989.中国钼矿床.宋叔和主编,中国矿床.北京：地质出版社,482-512
黄典豪,吴澄宇,杜安道,等.1994.东秦岭地区钼矿床的铼-锇同位素年龄及其意义.矿床地质,13(3)：221-230
黄典豪,杜安道,吴澄宇,刘兰笙,孙亚莉,邹晓秋.1996.华北地台钼(铜)矿床成矿年代学研究.矿床地质,15(4)：365-373
黄凡,罗照华,卢欣祥,高飞,陈必河,杨宗锋,潘颖,李德东.2009.东沟含钼斑岩由太山庙岩基派生?矿床地质,(5)：569-584
黄建军,黄楚秀.1985.陕西小秦岭地区钼的区域地球化学场的分布特征与矿化关系.河南地质,3(增刊)：128-134
贾承造,施央申.1986.东秦岭燕山期A型板块俯冲带的研究.南京大学学报,22(1)：120-128
黎世美,曹庆臻,吴国昌.1985.河南栾川上房沟夕卡岩—斑岩型钼(铁)矿床的围岩蚀变与矿化特征.河南地质,3(增刊)：259-266
黎世美,瞿伦全,李新民,等.1993.熊耳山地区蚀变构造岩型金矿成矿地质条件富集规律成矿模式及远景预测.北京：地质出版社,96-132
黎世美,瞿伦全,苏振邦,黄建军,王小生,岳铮生.1996.小秦岭金矿地质和成矿预测.北京：地质出版社,57-174
李立,杨辟元,段波,李艳军,金国元,钟清,刘玉华,万明浩,高平.1998.东秦岭岩石层的地电模型.地球物理报,41(2)：189-196
李红艳,毛景文,孙亚莉,邹晓秋,何红蓼,杜安道.1996.柿竹园钨多金属矿床的Re-Os同位素等时线年龄研究.地质论评,42(3)：261-267
李厚民,王登红,张冠,陈毓川,王彦斌,张长青,代军治.2007.河南白石坡银矿区花岗斑岩中锆石的SHRIMP U-Pb年龄及其地质意义.地质学报,81(6)：808-813
李厚民,叶会寿,王登红,陈毓川,屈文俊,杜安道.2009.豫西熊耳山寨凹钼矿床辉钼矿铼-锇年龄及其地质意义.矿床地质,(2)：133-142
李济营,张云政,瓮纪昌,吕伟庆.2010.河南汝阳东沟钼矿床下铺花岗斑岩体特征及其控矿作用.地质调查与研究,33(3)：
李晶,陈衍景,李强之,唐国军.2004.东秦岭上宫金矿流体成矿作用：矿物学研究.矿物岩石,24(3)：28-35
李莉,齐金忠.2002.河南公峪石英脉型金矿地质特征及其成因探讨.矿床地质,21卷增刊：
李诺,孙亚莉,李晶,薛良伟,2008a.小秦岭大湖金钼矿床辉钼矿铼锇同位素年龄及印支期成矿事件.岩石学报,24(4)：810-816
李诺,赖勇,鲁颖淮,郭东升.2008b.河南祁雨沟金矿流体包裹体及矿床成因类型研究.35(6)：1230-1239
李诺,陈衍景,孙亚莉,胡海珠,李晶,张辉.2009.河南鱼池岭钼矿床辉钼矿铼-锇同位素年龄及地质意义.岩石学报,25(2)：413-421
李齐,王瑜,万景林,李大明,王非.2001.秦岭造山带中段中新生代构造抬升的热年代学证据.矿物岩石地球化学通报,20(4)：263-265
李三忠,刘建忠,赵国春,吴福元,韩宗珠,杨中柱.2004.华北克拉通东部地块中生代变形的关键时限及其对构造的制约-以胶辽地区为例.岩石学报,20(3)：633-646
李曙光,Hart S R,郭安林,等.1987.河南中部登封群全岩Sm-Nd同位素年龄及其构造意义.科学通报,(22)：1728-1731
李树臣,周利霞.2008.山西省灵丘县支家地铅锌银矿床地质特征及成矿预测.地质与勘探,44(3)：18-21
李先梓,严阵,卢欣祥.1993.大秦-大别山花岗岩.北京：地质出版社,1-216
李祥才,董绍忠,张志伟,马建德.2001.万银坑银多金属矿地质特征及成因探讨.有色矿冶,17(6)：1-4
李永峰,毛景文,白凤军,李俊平,和志军.2003.东秦岭南泥湖钼矿Re-Os同位素年龄及其地质意义.地质论评,49(6)：652-659
李永峰,毛景文,郭保健,白凤军.2004.豫西公峪金矿床地质地球化学特征及成因探讨.矿床地质,23(1)：61-66
李永峰,毛景文,胡华斌,白凤军,李厚民,李蒙文,郭保健,叶会寿.2005.豫西公峪金矿床流体包裹体及其He.Ar.S.H.O同位素组成对成矿流体来源的示踪.岩石学报,21(5):1347-1358
李永峰,毛景文,刘敦一,王彦斌,王志良,王义天,李晓峰,张作衡,郭保健.2006.豫西雷门沟斑岩钼矿SHRIMP锆石U-Pb及辉钼矿Re-Os测年及其地质意义.地质论评,52(1)：122-131
李振国,年平国.2009.河南省罗山县白石坡银多金属矿床地质特征及成矿规律分析.现代矿业,(5)：85-87
李志昌等.1988.衫-钕法实验条件研究和地质应用.中国地质科学院宜昌地质矿产研究所所刊,第13号,1-23
梁钢.1995.江西万年虎家尖银金矿床地质特征及矿床成因初探.江西地质,9(1)：52-61
刘敦一.2002.SHRIMP技术及其在中国的首次登陆.地质通报,21(1)：53
刘国惠,张寿广,游振东,等.1993.秦岭造山带主要变质岩群及其变质演化.北京：地质出版社,26-84
刘国营,刘国庆.2009.青岗坪金矿床地质特征及成因探讨.桂林工学院学报,29(3)：323-326
刘灵恩,胡国民,支凤歧.2004.豫西寨凹隐伏岩体对周边银多金属矿的控矿作用.矿产与地质,18(1)：31-34
刘灵恩,王永争,刘金平.2011.矿化率在商业性地质勘查开发中的应用探讨.矿产勘查,待刊
刘灵恩,翟东兴,李红超,张侍威.2011.豫西沙沟-月亮沟矿区薄脉型铅锌银矿床地质特征及勘查实践经验总结.矿产勘查,待刊
刘荣绰,张泰华.1981.三道庄层状夕卡岩钼钨矿床的一般特征.河南地质,(1)：11-22
刘孝善,严正富,郑素娟,武耀成,黄标,吴澄宇.1987.东秦岭有色金属成矿带中典型矿床赋矿地层的地质地球化学研究.矿床地质,6(4)：1-10
刘孝善,孙晓明.1989.金堆城铝矿床成矿流体包裹体及稳定同位素研究.地质与勘探,25(2)：12-20
刘勇胜,袁洪林,高山,胡兆初,王选策,柳小明,凌文黎.2004.汉诺坝橄榄辉石岩包体锆石U-Pb年龄：97-158 Ma岩浆底侵作用和麻粒岩相变质作用之间的成因联系.科学通报,49(8)：790-797
娄德波,肖克炎,丁建华,孙艳.2010.矿产资源评价系统(MRAS)在全国矿产资源潜力评价中的应用.地质通报,29(11)：1677-1684.
卢欣祥,孔大刚.1982.河南省秦岭-大别山地区燕山期主要中酸性小岩体硫同位素组成特征.河南地质,1982(2)：7-12
卢欣祥.1983.河南省秦岭-大别山地区燕山期中酸性小岩体的基本地质特征及成矿专属性.河南地质,1(1)：49-55
卢欣祥.1988.龙王石童碱性花岗岩——东秦岭最大A型花岗岩的地质矿化特征及意义.见：张国伟等著.秦岭造山带的形成与其演化.西安：西北大学出版社,135-147
卢欣祥,董有,常秋岭,肖庆辉,李晓波,王晓霞.1996.秦岭印支期沙河湾奥长环斑花岗岩及其动力学意义.中国科学(D辑),26(30)：244-248
卢欣祥.1999.秦岭花岗岩大地构造图.西安：西安地图出版社
卢欣祥,于在平,冯有利,王义天,马维峰,崔海峰.2002.东秦岭深源浅成型花岗岩的成矿作用及地质构造背景.矿床地质,21(2)：168-178
卢欣祥,尉向东,董有,于在平,常秋玲,等.2004.小秦岭-熊耳山地区金矿特征与地幔流体.北京：地质出版社,102-119
陆松年,李怀坤,陈志宏,等.2003.秦岭中-新元古代地质演化及对Rodinia超级大陆事件的响应.北京：地质出版社,163-174
陆松年,陈志宏,李怀坤,郝国杰,周红英,相振群.2004.秦岭造山带中-新元古代(早 期)地质演化.地质通报,23(2)：107-112
栾世伟,陈尚迪,等.1991.小秦岭地区深部金矿化特征及评价.成都：成都科技大学出版社
罗铭玖.1981.河南斑岩钼矿矿化分带、矿床型式及成矿规律初探.河南地质,(1)：1-10
罗铭玖,董群英,李兴福,李昆华.1985.河南栾川南泥湖-三道庄钼钨矿床的地质特征及矿床类型.河南地质,3(增刊)：237-245
罗铭玖,张辅民,董群英,等.1991.中国钼矿床.郑州：河南科学技术出版社,118-408
罗铭玖,黎世美,卢欣祥,郑德琼,苏振邦.2000.河南省主要矿产的成矿作用及矿床成矿系列.北京：地质出版社,244-287
罗平,魏英文,王永庆.2005.北武夷长寿源银铅(锌)矿床地质特征.资源调查与环境,26(1)：33-42
吕庆田,侯增谦,赵金花,史大年,吴宣志,常印佛,裴荣富,黄东定,匡朝阳.2003.深地震反射剖面揭示的铜陵矿集区复杂地壳结构形态.中国科学(D辑),33(5)：442-449
吕庆田,侯增谦,杨竹森,史大年.2004.长江中下游地区的底侵作用及动力学演化模式：来自地球物理资料的约束.中国科学(D辑),34(9)：783-794
吕仁生.1987.三道庄钼钨矿床矿液流向的研究.河南地质,5(3)：14-18
吕文德,孙卫志,王喜恒,肖中军,徐文超,杨国强.2002.河南省栾川赤土店地区银铅锌成矿地质条件及找矿前景.前寒武纪研究进展,25(3-4)：165-169
吕文德,孙卫志.2004.卢氏-栾川地体铅锌矿成矿地质条件分析及找矿远景.矿产与地质,18(6)：507-516
吕文德,赵春和,孙卫志,燕建设.2005.河南栾川地区矽卡岩型铅锌矿地质特征——南泥湖钼矿外围找矿问题.地质调查与研究,28(1)：25-31
毛景文,王志良.2000.中国东部大规模成矿时限及其动力学背景的初步探讨.矿床地质,19(4)：289-296
毛景文,张作衡,余金杰,王义天,牛宝贵.2003.华北及邻区中生代大规模成矿的地球动力学背景：从金属矿床年龄精测得到启示.中国科学(D辑),33(4)：289-299
毛景文,李晓峰,张荣华,王义天,赫英,张作衡,等.2005.深部流体成矿系统.北京：中国大地出版社,5-11
毛景文,郑榕芬,叶会寿,高建京,陈文.2006.豫西熊耳山地区沙沟银铅锌矿床成矿的40Ar-39Ar年龄及其地质意义.矿床地质,25(4)：359-368
倪师军.1994.小秦岭中基性岩脉秘金矿成因关系新模式.西安：西安交通大学出版社,1-132
倪志耀,王仁民,童英,杨淳,戴潼谟.2003.河南洛宁太华岩群斜长角闪岩的锆石207Pb/206Pb和角闪石40Ar/39Ar年龄.地质论评,49(4)：361-366
倪智勇,李诺,管申进,张辉,薛良伟.2008河南小秦岭金矿田大湖金-钼矿床流体包裹体特征及矿床成因.岩石学报,24(9)：2058-2068
倪智勇,李诺,张辉,薛良伟.2009.河南大湖金钼矿床成矿物质来源的锶钕铅同位素约束.岩石学报,25(11)：2823-2832
裴荣富.1995.中国矿床模式.北京：地质出版社,1-120
裴先治,李厚民,李国光.1996.东秦岭商丹断裂带南侧变质基性岩的时代和岩石地球化学特征.西北地质科学,16(2)：49-57
裴先治.1997.东秦岭商丹构造带的组成与构造演化.西安：西安地图出版社,1-133
裴先治,王涛,王洋,李厚民,李国光.1999.北秦岭晋宁期主要地质事件及其构造背景探讨.高校地质学报,5(2)：137-147
彭恩生.1994.篙坪沟-铁炉坪地区银金多金属矿床成矿地质特征.中南矿冶学院学报,25(4)：427-430
彭万夫.1981.秦岭东段中酸性小岩体岩石化学成分的演化特征及与以钼为主的成矿关系.河南地质,(4)：1-13.
彭万夫.1986.秦岭-大别山区燕山期中酸性小岩体岩石化学成分及含矿性.河南地质,4(3)：1-13
齐金忠,马占荣,李莉.2004.河南祁雨沟金矿床成矿流体演化特征.黄金地质,10(4)：1-10
祁进平,宋要武,李双庆,陈福坤.2009.河南省栾川县西沟铅锌银矿床单矿物铷-锶同位素组成特征.岩石学报,25(11)：2843-2854
乔怀栋,刘长命,董有,彭万夫.1983.初步探讨东秦岭地区与小岩体有关矿床的成矿模式.河南地质,1(1)：25-34
任富根,李维明,李增慧,等.1996.熊耳山-崤山地区金矿成矿地质条件和找矿综合评价模型.北京：地质出版社,1-120
任富根,李惠民,殷艳杰,李双保,丁士应,陈志宏.2000.熊耳群火山岩系的上限年龄及其地质意义.前寒武纪研究进展,23(3)：140-146
任富根,殷艳杰,李双宝,赵嘉农.2001.熊耳裂陷印支期同位素地质年龄耦合性.矿物岩石地球化学通讯,20(4)：286-288
任富根,李惠民,殷艳杰,李双保,丁士应,陈志宏.2002.豫西地区熊耳群的地质年代学研究.前寒武纪研究进展,25(1)：41-47
陕西省地质矿产局,1989.陕西省区域地质志.北京：地质出版社,1-700
邵克忠,王宝德,吴新国,等.1992.祁雨沟地区爆发角砾岩型金矿成矿地质条件及找矿方向研究.河北地质学院学报,15(2)：105-194
盛中烈,罗铭玖,李良骏.1980.豫西斑岩钼矿带的基本地质特征及主要成矿控制因素.地质学报,54(4)：300-309
盛中烈,温明星,隋慎范.1984.东秦岭钼多金属成矿带内地层在成矿过程中的作用.河南地质,2(1)：23-28
施俊法,肖庆辉.2004.经验勘查与理论勘查的发展趋势.地质通报,23(8)：809-815
石铨曾,尉向东,李明立.1995.小秦岭变质核杂岩基本特征及与金的成矿作用.河南地质矿产与环境论文集,1-196
石铨曾,陶自强,庞继群,曲明绪.1996.华北板块南缘栾川群研究.华北地质矿产杂志,11(1)：51-59
石铨曾,尉向东,李明立,庞继群.2004.河南省东秦岭山脉北缘的推覆构造及伸展拆离构 造.地质出版社,1-202
隋颖慧,王海华,高秀丽,陈华勇,李震.2000.河南铁炉坪银矿成矿流体研究及其对碰撞造山成岩成矿与流体作用模式例证.中国科学(D辑),30(增刊)：82-90
孙敏,张立飞,吴家弘.1996.早元古代宽甸杂岩的成因：地球化学证据.地质学报,70(3)：207-222
孙枢,从柏林,李继亮.1981.豫、陕中、晚元古代沉积盆地.地质科学,(4)：314-322
孙枢,张国伟,陈志明.1985.华北断块区南部前寒武纪地质演化.冶金工业出版社,1-216
孙晓明,刘孝善.1987.金堆城钼矿区两类不同花岗岩的关系及其成因研究.地质找矿论丛,2(2)：34-44
孙晓明,任启江,杨荣勇,徐兆文,刘孝善.1998.金堆城超大型钼矿床水-岩δD-δ18O同位素交换体系理论模型及成矿流体来源.地质地球化学,26(2)：16-21
孙勇,卢欣祥,韩松,张国伟,杨司祥.1996.北秦岭早古生代二郎坪蛇绿岩片的组成和地球化学.中国科学(D辑),26(增刊)：49-55
宋国耀,张晓华,肖克炎.矿产资源潜力评价的理论和GIS技术[R]
宋国耀,张晓华,肖克炎.1999.矿产资源潜力评价的若干问题[J].中国地质,1999.
王非,朱日祥,李齐,贺怀宇,罗清华,卢欣祥,桑海清,王英兰.2004.秦岭造山带的差异隆升特征——花岗岩10Ar-39Ar年代学研究的证据.地学前缘,11(4)：445-459
王海华,陈衍景,高秀丽.2001.河南省康山金矿同位素地球化学及其对成岩成矿及流体作用模式的印证.矿床地质,20(2)：190-198.
王昊,徐刚,路坦,刘旭,瞿东旭.2007.河南省银洞沟银多金属矿床地质特征及成因分析.矿产与地质,21(4)：429-435
王家枢,曹新元.2009.对矿产勘查工作规律的初步分析和归纳.国土资源情报,7：6-12
王天聪.1985.雷门沟钼矿床地质特征.河南地质,3(增刊)：270-272
王义天,毛景文,卢欣祥.2001.嵩县祁雨沟金矿成矿时代的40Ar/39Ar年代学证据.地质论评,47(5)：551-555
王义天,毛景文,卢欣祥,叶安旺.2002a.河南小秦岭金矿区Q875脉中深部矿化蚀变岩的40Ar/39Ar年龄及其意义.科学通报,47(18)：1427-1431
王义天,毛景文.2002b.碰撞造山作用期后仲展体制下的成矿作用—以小秦岭金矿集中区为例.地质通报,21(8-9)：562-566
王义天,毛景文,叶安旺,叶会寿,李永峰,卢欣祥,李永革.2005.小秦岭地区中深部含金石英脉的同位素地球化学特征及其意义.矿床地质,24(3)：270-279
王跃峰.2000.栾川群大红口组火山岩研究初探.河南地质,18(3)：181-189
王志光,崔毫,徐孟罗,等.1997.华北地块南缘地质构造演化与成矿.北京：冶金工业出版社,1-296
王作勋等.1995.秦岭造山带显生宙构造迁移与陶湾群沉积变形.北京：地震出版社
王浩丞,孙宝生.2010.矿产资源潜力评价研究现状及发展方向展望.西部探矿工程,2010(10)：165-166
魏庆国,姚军明,赵太平,孙亚莉,李晶,原振雷,乔波.2009.东秦岭发现-1.9(a钼矿床 -河南龙门店钼矿床Re-Os定年.岩石学报,25(11)：2747-2751
温森坡.2008.嵩县店房火山角砾岩体西段金成矿潜力分析.黄金,29(12)：15-18
吴福元,孙德有.1999.中国东部中生代岩浆作用与岩石圈减薄.长春科技大学学报,29(4)：313-318
吴福元,孙德有,张广良,任向文.2000.论燕山运动的深部地球动力学本质.高校地质学报,6(3)：379-388
吴华,李华芹,莫新华,陈富文,路远发,梅玉萍,邓岗.2005.新疆哈密白石泉铜镍矿区基性-超基性岩的形成时代及其地质意义.地质学报,79(4)：498-502
吴良士,邹晓秋.1997.江西城门山铜矿铼-锇I司位素年龄研究.矿床地质,16(4)：376-381
肖克炎,张晓华,王四龙,等.2000.矿产资源GIS评价系统.北京：地质出版社,142
肖克炎,张晓华,李景朝.2007.全国重要矿产总量预测方法[J].地学前缘,2007,14(5)：20-26.
肖克炎,丁建华,刘锐.2005.美国“三步式”固体矿产资源潜力评价方法评述[J].地质论评,2006,52(6)：793-798.
徐国风.1985.论豫西银家沟钼-铜-硫铁矿矿床的矿质来源.河南地质,3(增刊)：266-270
徐启东,钟增球,周汉文,杨发城,唐学超.1998.豫西小秦岭金矿区的一组40Ar/39Ar定年数据.地质论评,44(3)：323-327
徐士进.1985.河南栾川上房沟细脉浸染钼矿床围岩蚀变与成矿作用的关系及其地球化学特征.河南地质,3(4)：33-42
徐文超,庞振山,周奇明,王喜恒,杨国强.2003.河南省栾川县南泥湖钼钨矿田外围银铅锌多金属成矿地质条件分析及找矿前景.矿产与地质,17(3)：198-202
徐兆文,杨荣勇,刘红樱,陆现彩,徐文艺,任启江.1998a.陕西金堆城斑岩钼矿床成矿流体研究.高校地质学报,4(4)：423-431
徐兆文,杨荣勇,陆现彩,任启江.1998b.金堆城斑岩钼矿床地质地球化学特征及成因.地质找矿论丛,13(4)：18-27
许永仁.1985.洛南-豫西斑岩钼矿带控岩控矿构造环境初步分析.河南地质,3(增刊)：135-139
许志琴,卢一伦,汤耀庆,M. Mattaure, Ph. Matte, J. Malavieille, P. Tapponnier, H. Maluski.1986.东秦岭造山带的变形特征及构造演化.地质学报,60(3)：237-247
薛良伟,原振雷,张荫树,强立志.1995.鲁山太华岩群Sm-Nd司位素年龄及其意义.地球化学,24(增刊)：92-97
严正富,杨正光,程海,杨浩,付成义,吴智慧.1986.雷门沟钼矿化花岗斑岩成因浅析.南京大学学报,22(3)：525-535
燕长海,刘国印,宋锋,张正伟.2002.河南马超营-独树一带银铅锌成矿地质条件及找矿前景.中国地质,29(3)：305-310
燕长海,刘国印,邓军.2003.豫西南铅锌银矿集区深部构造与成矿作用.地质调查与研究,26(4)：221-227
燕长海,宋要武,刘国印,邢矿.2004a.河南栾川杨树凹-百炉沟MVT铅锌矿带地质特征.地 质调查与研究,27(4)：249-254
燕长海,刘国印.2004b.豫西南铅锌多金属矿控矿条件及找矿方向.地质通报,23(11)：1143-1148
燕长海.2004c.东秦岭铅锌银成矿系统内部结构.北京：地质出版社,46-96
杨进朝,冯胜斌,彭翼,燕长海,曾宪友,王建明,胡绍斌.2008.豫西嵩县上庄坪铅锌银矿床地球化学特征及地质意义.中国地质,35(02)：305-309
杨经绥,许志琴,斐先治,史仁灯,吴才来,张建新,李海兵,孟繁聪,戎合.2002.秦岭发现金刚石横贯中国中部巨型超高压变质带新证据及古生代和中生代两期深俯冲作用的识别.地质学报,76(4)：484-495
杨忆.1983.熊耳群钾质细碧-石英角斑岩岩石特征及成因探讨.1981届硕士学位论文集.北京：科学出版社
杨忆.1990.华北地台南缘熊耳群火山岩特点及形成的构造背景.岩石学报,(2)21-28
杨正光,严正富.1985.雷门沟钼矿化花岗斑岩特征及其成因系列的探讨.河南地质,3(增刊)：273-278
姚瑞增.1986.洛南.豫西斑岩钼矿带成岩成矿构造作用浅析.河南地质,4(4)：14-19
叶天竺.2012.固体矿产找矿预测方法研究纲要.内部资料
叶会寿,毛景文,李永峰,燕长海,郭保健,赵财胜,何春芬,郑榕芬,陈莉.2006a.豫西南泥湖矿田钼钨及铅锌银矿床地质特征及其成矿机理探讨.现代地质,20(1)：165-174
叶会寿,毛景文,李永峰,郭保健,张长青,刘珺,闫全人,刘国印.2006b.东秦岭东沟斑岩SHRIMP锆石U-Pb年龄和钼矿Re-Os年龄及其地质意义.地质学报,80(5)：1078-1088
叶玉丰.2004.基于GIS技术的矿产资源规划管理信息系统[J].地质与资源,2004,13(1)52-64.
袁学诚,徐明才,唐文榜等.1994.东秦岭陆壳反射地震剖面.地球物理学报,37(6)：749-758
袁跃清,王秀全,冯昂.2005.河南省西部四道沟银-铅矿区地质特征及找矿远景分析.矿产与地质,19(4)：371-374
曾华杰,张泰华,张炳欣,宋北城.1983.南泥湖钼矿田同熔型花岗岩类的成因研究.河南地质,1(1)：56-66.
曾华杰,张炳欣.1985.河南栾川南泥湖钼矿田矿床地质特征及其成因探讨.河南地质,3(增刊)：46-250
翟明国.2010.华北克拉通的形成演化与成矿作用.矿床地质,29(1)：24-36
翟裕生.1999.论成矿系统.地学前缘,6(1)：13-26
张本仁,骆庭川,高山,欧阳建平,陈德兴,马振东,韩吟文,谷晓明,等.1994.秦巴岩石圈构造及成矿规律地球化学研究.武汉：中国地质大学出版社,257-364
张本仁,张宏飞,赵志丹,凌文黎.1996.东秦岭及邻区壳、幔地球化学分区和演化及其大地构造意义.中国科学(D辑),26(3)：201-208
张本仁,高山,张宏飞,韩吟文,等.2002.秦岭造山带地球化学.北京：科学出版社,1-173
张德会.1997.成矿流体中金的沉淀机理研究述评.矿物岩石,17(4)：122-130
张国伟,孟庆任,于在平,孙勇,周鼎武,郭安林.1996.秦岭造山带的造山过程及其动力学特征.中国科学(D辑),26(3)：193-200
张国伟,张本仁,袁学诚,肖庆辉,等.2001.秦岭造山带与大陆动力学.北京：科学出版社,1-806
张进江,郑亚东,刘树文.1998.小秦岭变质核杂岩的构造特征、形成机制及构造演化.北京：海洋出版社,17-63.
张洪岩,王软敏,周成虎,等.2001.“数字地球”与地理信息科学[J].地球信息科
学,2001(4)：124.
张理刚.1989.成岩成矿理论与找矿—中国主要类型矿床及花岗岩类的稳定同位素地质学.北京：北京科技大学出版社,143
张理刚,刘敬秀,王可法,等.1995.东亚岩石圈块体地质-上地幔、基底和花岗岩同位素地球化学及其动力学.北京：科学出版社
张连昌,沈远超,李厚民,曾庆栋,李光明,刘铁兵.2002.胶东地区金矿床流体包裹体的He、Ar同位素组成及成矿流体来源示踪.岩石学报,18(4)：559-565
张乃昌,阎景汉,刘新年.1986.从重磁成果探讨我省深部构造及成矿作用.河南地质,4(1)：16-22.
张旗,张宗清,孙勇,韩松.1995.陕西商县-丹凤地区丹凤群变质玄武岩的微量元素和同位素地球化学.岩石学报,11(1)：43-54
张天义,王俊卿.1996.熊耳山、外方山地区金矿成矿条件的遥感地质特征.关保德著,河南华北地台南缘前寒武世地质和成矿,118-133。
张天义,朱嘉伟,盛吉虎.1997.秦岭大地构造格局的遥感地质分析.河南地质,15(3)：179-185
张瑜麟.2001.熊耳山银铅成矿区物探找矿方法应用研究.地质与勘探,37(6)：46-50
张瑜麟.2003.熊耳山西段银铅矿找矿地球物理标志研究.矿产与地质,2003
张正伟,朱炳泉,常向阳.2000.东秦岭北部富碱侵入岩钕、锶、铅同位素特征及构造意义.地球化学,29(5)：455-461
张正伟,邓军.2001.东秦岭钼矿带成矿背景与含矿岩体特征.陈衍景,张静,赖勇主编.大陆动力学与成矿作用.北京：地震出版社,100-109
张正伟,朱炳泉,常向阳.2003.东秦岭北部富碱侵入岩带岩石地球化学特征及构造意义.地学前缘,10(4)：507-519
张宗清,刘敦一,付国民.1994.北秦岭变质地层同位素年代研究.北京：地质出版社,1-200
张宗清,张国伟,唐索寒,广欣祥.1999.秦岭沙河湾奥长环斑花岗岩的年龄及其对秦岭造山带主造山期结束时问的限制.科学通报,44(9)：981-984
张宗清,张国伟,唐索寒.2002.南秦岭变质地层同位素年代学.北京：地质出版社,1-123
赵书梅.2008.多种地质找矿手段的综合应用.硅谷,19：4
赵太平,庄建敏,原振雷.1996.华北板块南缘熊耳群火山岩岩石类型及火山岩系列.华北地质矿产杂志,11(4)：599-606
赵太平,周美夫,金成伟,关鸿,李惠民.2001.华北陆块南缘熊耳群形成时代讨论.地质科学,36(3)：326-334
赵太平,金成伟,翟明国,夏斌,周美夫.2002.华北陆块南部熊耳群火山岩的地球化学特征与成因.岩石学报,18(1)：59-69
赵太平,翟明国,夏斌,李惠民,张毅星,万渝生.2004.熊耳群火山岩锆石SHRIMP年代学研究：对华北克拉通盖层发育初始时间的制约.科学通报,49(22)：2342-2349
赵振华,涂光炽.2003.中国超大型矿床(Ⅱ).北京：科学出版社,523-542
郑建平,路凤香,郭晖,任迎新.1994.金刚石中流体包裹体的研究.科学通报,39(3)：253-256
郑榕芬,毛景文,高建京.2004.河南熊耳山沙沟银铅锌矿床中硫化物和银矿物的矿物学特征及其意义.矿床地质,25(6)：715-726
支风岐,刘灵恩,索勇.2004.河南省熊耳山西段沙沟西银铅矿区地质特征及找矿前景分析.矿产与地质,18(1)：35-38
周珂,叶会寿,毛景文,屈文俊,周树峰,孟芳,高亚龙.2009.豫西鱼池岭斑岩型钼矿床地质特征及其辉钼矿铼-锇同位素年龄.矿床地质,28(2)：170-184
朱炳泉.1993.矿石铅同位素三维拓扑图解用于地球化学省与矿种区划.地球化学,22(3)：209-216
朱炳泉.1998.壳幔化学不均一性与块体地球化学边界研究.地学前缘,5(1-2)：72-82
朱嘉伟,张天义,薛良伟.1999.豫西崤山地区金矿成矿年龄的测定及其意义.地质论评,45(4)：418-422
朱裕生,王柏钧.矿产资源评价的现状和展望[R]
© 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 |