川西长征穹窿高分异花岗岩地球化学、锆石U-Pb定年、Lu-Hf同位素特征：对区域稀有金属成矿背景的限定
|
摘要
新近在川西松潘-甘孜造山带东南缘长征穹窿发现一处花岗伟晶岩型铷铍矿产地。为阐明与成矿花岗伟晶岩具密切成因关系的花岗岩的特征及其成矿背景,在详细野外地质调查的基础上,采集穹窿核部出露的花岗岩样品开展了镜下鉴定、元素地球化学及锆石LA-(MC)-ICP-MS U-Pb和Lu-Hf同位素测试工作。结果表明,长征穹窿核部出露的两处花岗岩岩枝分别由二长花岗岩和正长花岗岩组成,岩石高硅、富铝、高钾、富碱、低钙、低Na/K比值,为高钾钙碱性岩石系列,A/CNK值均大于1.1,为过铝质花岗岩;岩石相对富集大离子亲石元素K、Rb和放射性元素U,而亏损Ba、Sr、Ti等微量元素;岩石稀土元素总量为30.9×10~(-6)～69.0×10~(-6),LREE/HREE为4.2～8.0,轻稀土元素富集明显,δEu为0.12～0.57,具明显的负铕异常;锆石U-Pb定年结果分别为(202.2±1.3)Ma(MSWD=0.42,n=15)和(202.2±1.5)Ma(MSWD=1.18,n=9),长征穹窿核部花岗岩岩浆结晶时代为晚三叠世末期;锆石Lu-Hf同位素ε_(Hf)(t)和T_(DM2)分别为-15.42～-4.71和2.22～1.54 Ga,花岗岩可能起源于下地壳。综合分析认为,长征穹窿核部花岗岩为典型的高分异花岗岩,源于下地壳的初始岩浆在晚三叠世末期上升侵位过程中混染了较多围岩成分而形成;区域伟晶岩至少存在3期成矿作用,稀有金属矿化为多期或多次岩浆作用的产物,预测区域可能存在一期194 Ma左右的伟晶岩稀有金属成矿事件;区域与稀有金属成矿作用有关的花岗岩为多期或多次岩浆作用晚期的产物,形成于同碰撞构造向碰撞后伸展构造转换的相对稳定环境。
A granite-pegmatite-type rubidium-beryllium orefield has recently been discovered in the Changzheng dome on the southeastern margin of the Songpan-garzê orogenic belt in western Sichuan. In order to clarify the metallogenic geological background, the authors collected granite samples in the dome core which is closely related to the generation of mineralized granite pegmatite for microscopic identification, element geochemistry and zircon LA-(MC)-ICP-MS U-Pb and Lu-Hf isotope testing on the basis of detailed field geological survey. The results show that the two granites in the core of the Changzheng dome are syenogranite and monzonite, characterized by high silicon, aluminium, potassium, alkali, low calcium and low Na/K ratios. They belong to high potassium calc-alkaline rock series. the A/CNK ratios are all higher than 1.1, suggesting peraluminous granites. The rocks are relatively enriched in large ion lithophile elements K, Rb and radioactive elements U, but depleted in trace elements such as Ba, Sr and Ti. The ΣREE is 30.9×10~(-6)～69.0 ×10~(-6), and LREE/HREE is 4.2～8.0, with obvious enrichment of light REE elements. The δEu is 0.12～0.57, with obvious negative Eu anomaly. The zircon U-Pb dating results are(202.2+1.3) Ma(MSWD=0.42, n=15) and(202.2+1.5) Ma(MSWD=1.18, n=9), suggesting that the magmatic crystallization of granite in the core of the Changzheng dome took place at the end of Late Triassic,and its zircon Lu-Hf isotope epsilon ε_(Hf)(t) and T_(DM2) are-15.42～-4.71 and 2.22～1.54 Ga, respectively. Comprehensive analysis shows that the granite in the core of the Changzheng dome is a typical highly differentiated granite.The initial magma originated from the lower crust mixed with surrounding rock components in the process of ascending emplacement at the end of the Late Triassic period. There existed at least three stages of mineralization of pegmatite in the study area. The rare metals are the products of multiphase magmatism and the authors hold that there probably existed a pegmatite rare metal metallogenic event at ± 194 Ma in the study area. The regional granites related to rare metal metallogenesis were formed in late-stage of multiphase magmatism and formed in relatively stable environments such as conversion process from syn-collisional to post-collisional extensional tectonic environment.
A granite-pegmatite-type rubidium-beryllium orefield has recently been discovered in the Changzheng dome on the southeastern margin of the Songpan-garzê orogenic belt in western Sichuan. In order to clarify the metallogenic geological background, the authors collected granite samples in the dome core which is closely related to the generation of mineralized granite pegmatite for microscopic identification, element geochemistry and zircon LA-(MC)-ICP-MS U-Pb and Lu-Hf isotope testing on the basis of detailed field geological survey. The results show that the two granites in the core of the Changzheng dome are syenogranite and monzonite, characterized by high silicon, aluminium, potassium, alkali, low calcium and low Na/K ratios. They belong to high potassium calc-alkaline rock series. the A/CNK ratios are all higher than 1.1, suggesting peraluminous granites. The rocks are relatively enriched in large ion lithophile elements K, Rb and radioactive elements U, but depleted in trace elements such as Ba, Sr and Ti. The ΣREE is 30.9×10~(-6)～69.0 ×10~(-6), and LREE/HREE is 4.2～8.0, with obvious enrichment of light REE elements. The δEu is 0.12～0.57, with obvious negative Eu anomaly. The zircon U-Pb dating results are(202.2+1.3) Ma(MSWD=0.42, n=15) and(202.2+1.5) Ma(MSWD=1.18, n=9), suggesting that the magmatic crystallization of granite in the core of the Changzheng dome took place at the end of Late Triassic,and its zircon Lu-Hf isotope epsilon ε_(Hf)(t) and T_(DM2) are-15.42～-4.71 and 2.22～1.54 Ga, respectively. Comprehensive analysis shows that the granite in the core of the Changzheng dome is a typical highly differentiated granite.The initial magma originated from the lower crust mixed with surrounding rock components in the process of ascending emplacement at the end of the Late Triassic period. There existed at least three stages of mineralization of pegmatite in the study area. The rare metals are the products of multiphase magmatism and the authors hold that there probably existed a pegmatite rare metal metallogenic event at ± 194 Ma in the study area. The regional granites related to rare metal metallogenesis were formed in late-stage of multiphase magmatism and formed in relatively stable environments such as conversion process from syn-collisional to post-collisional extensional tectonic environment.
引文
Andersen T.2002.Correction of common Pb in U-Pb analyses that do not report 204Pb[J].Chemical Geology,192(1):59-79.
Bakker R J and Elburg M A.2006.A magmatic-hydrothermal transition in Arkaroola(northern Flinders Ranges,South Australia):From diopside-titanite pegmatites to hematite-quartz growth[J].Contributions to Mineralogy and Petrology,152(5):541-569.
Barbarin B.1999.A review of the relationships between granitoid types,their origins and their geodynamic environments[J].Lithos,46(3):605-626.
Bau M.1996.Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems:Evidence from Y/Ho,Zr/Hf,and lanthanide tetrad effect[J].Contributions to Mineralogy and Petrology,123(3):323-333.
Boynton W V.1984.Geochemistry of the rare earth elements:Meteoritestudies[A].In:Henderson P,ed.Rare earth element geochemistry[C].Amsterdam:Elsevier.63-114.
Cohen K M,Finney S C,Gibbard P L and Fan J X.2013.The ICSinternational chronostratigraphic chart[J].Episodes,36(3):199-204
Dill H G.2015.Pegmatites and aplites:Their genetic and applied ore geology[J].Ore Geology Reviews,69:417-561.
Fu X F,Hou L W,Wang D H,Yuan L P,Liang B,Hao X F and Pan M.2014.Achievements in the investigation and evaluation of Spodumene resources at Jiajika in Sichuan,China[J].Geological Survey of China,1(3):37-43(in Chinese with English abstract).
Fu X F,Yuan L P,Wang D H,Hou L W,Pan M,Hao X F,Liang B and Tang Y.2015.Mineralization characteristics and prospecting model of newly discovered X03 rare metal vein in Jiajika orefield,Sichuan[J].Mineral Deposits,34(6):1172-1186(in Chinese with English abstract).
Gao L E,Zeng L S,Hou K J,Guo C L,Tang S H,Xie K J,Hu G Y and Wang L.2013.Episodic crustal anatexis and the formation of Paiku composite leucogranitic pluton in the Malashan gneiss dome,southern Tibet[J].Chinese Science Bulletin,58(27):2810-2822(in Chinese with English abstract).
Guo S S and Li S G.2007.Petrological and geochemical constraints on the origin of leucogranites[J].Earth Science Frontiers,14(6):290-298(in Chinese with English abstract).
Gu C H.2014.Metallogenic regularity of spodumene deposits in the closely spaced pegmatite area in the southeastern Keeryin pegmatite field,Sichuan Province[J].Contributions to Geology and Mineral Resources Research,29(1):59-65(in Chinese with English abstract).
Hao X F,Fu X F,Liang B,Yuan L P,Pan M and Tang Y.2015.Formation ages of granite and X03 pegmatite vein in Jiajika,western Sichuan,and their geological significance[J].Mineral Deposits,34(6):1199-1208(in Chinese with English abstract).
Harris N B W and Inger S.1992.Trace element modelling of pelite-derived granites:Contributions to mineralogy and petrology[J].Contributions to Mineralogy and Petrology,110(1):46-56.
Hou L W and Fu X F.2002.Dome-shaped metamorphic geological body on the eastern margin of Songpan-Ganzi orogenic belt[M].Sichuan University Press(in Chinese).
Hu G Y,Zeng L S,Chen H and Gao L E.2016.Assembling mechanism for the Late-Miocene Mabja leucogranite pluton,Himalayan Orogen[J].Acta Geologica Sinica,90(8):1737-1754(in Chinese with English abstract).
Huang C M,Zhao Z D,Zhu D C,Liu D,Huang Y,Dong M C,Hu Z Cand Zheng J P.2013.Geochemistry,zircon U-Pb chronology and Hf isotope of Luozha leucogranite,southern Tibet:Implication for petrogenesis[J].Acta Petrologica Sinica,29(11):3689-3702(in Chinese with English abstract).
Hu J M,Meng Q R,Shi Y R and Qu H J.2005.SHRIMP U-Pb dating of zircons from granitoid bodies in the Songpan-Ganzi terrane and its implications[J].Acta Petrologica Sinica,21(3):867-880(in Chinese with English abstract).
Le Fort P.1973.Les leucogranitesàtourmaline de l’Himalaya sur l’exemple du granite du Manaslu(Népal central)[J].Bulletin de la Societe Geologique de France,15(5-6):555-561(in France).
Le Maitre R W.1989.A classification of igneous rocks and glossary of terms[M].Oxford:Black Well.
Li J K,Wang D H,Zhang D H and Fu X F.2006.The source of oreforming fluid in Jiajika pegmatite type lithium polymetallic deposit,Sichuan Province[J].Acta Petrologica et Mineralogica,25(1):45-52(in Chinese with English abstract).
Li X H,Li Z X,Li W X,Liu Y,Yuan C,Wei G J and Qi C S.2007.U-Pb zircon,geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I-and A-type granites from central Guangdong,SE China:A major igneous event in response to foundering of a subducted flat-slab[J]?Lithos,96(1):186-204.
Liang B,Fu X F,Tang Y,Pan M,Yuan L P and Hao X F.2016.Granite geochemical characteristics in Jiajika rare metal deposit,western Sichuan[J].Journal of Guilin University of Technology,36(1):42-49(in Chinese with English abstract).
Liu L J,Wang D H,Hou K J,Tian S H,Zhao Y,Fu X F,Yuan L P and Hao X F.2017.Application of lithium isotope to Jiajika new No.3pegmatite lithium polymetallic vein in Sichuan[J].Earth Science Frontiers,24(5):167-171(in Chinese with English abstract).
Liu Y D,Zhou Y,Guo R P,Zhou X and Zhang Y.2018.Anomalies characteristics of ground high-precision magnetic survey and the prospecting prediction in Jiajika style spodumene deposits,Sichuan[J].Mineral Exploration,9(3):428-437(in Chinese with English abstract).
London D and Morgan G B.2012.The pegmatite puzzle[J].Elements,8(4):263-268.
London D.2014.A petrologic assessment of internal zonation in granitic pegmatites[J].Lithos,184-187(1):74-104.
Ludwig K R.2003.Isoplot 3.0-A geochronological toolkit for Microsoft Excel.Berkeley geochronology center[M].Special Publication.(4):1-70.
Maniar P D and Piccoli P M.1989.Tectonic discrimination of granitoids[J].Geological Society of America Bulletin,101(5):635-643
Pati?o Douce A E and Harris N.1998.Experimental constraints on Himalayan anatexis[J].Journal of Petrology,39(4):689-710.
Pearce J A and Mei H.1988.Volcanic rocks of the 1985 Tibet Geotraverse:Lhasa to Golmud[J].Philosophical Transactions of the Royal Society of London,327(1594):169-201.
Pearce J A.1996.Sources and settings of granitic rocks[J].Episodes,19(4):120-125.
Rao K Y.2016.The geological characteristics and ore exploration targeting of Dilaqiu Lithium deposit in Maerkang County,Sichuan Provice[J].Sichuan Nonferrous Metals,25(1):54-57(in Chinese with English abstract).
Roger F,Calassou S,Lancelot J,Malavieille J,Mattauer M,Xu Z Q,Hao Z W and Hou L W.1995.Miocene emplacement and deformation of the Konga Shan granite(Xianshui He fault zone,West Sichuan,China):Geodynamic implications[J].Earth and Planetary Science Letters,130(1-4):201-216.
Roger F,Malavieille J,Leloup P H,Calassou S and Xu Z.2004.Timing of granite emplacement and cooling in the Songpan-GarzêFold Belt(eastern Tibetan Plateau)with tectonic implications[J].Journal of Asian Earth Sciences,22(5):465-481.
Roger F,Jolivet M and Malavieille J.2010.The tectonic evolution of the Songpan-Garzê(North Tibet)and adjacent areas from Proterozoic to Present:A synthesis[J].Journal of Asian Earth Sciences,39(4):254-269.
Rollinson H R.1993.Using geochemical date:Evaluation,presentation and interpretation[M].New York:Longman Group UK Ltd.
Su A N,Tian S H,Hou Z Q,Li J K,Li Z Z,Hou K J,Li Y H,Hu W Jand Yuan Z S.2011.Lithium isotope and its application to Jiajika pegmatite type lithium polymetallic deposit in Sichuan[J].Geoscience,25(2):236-242(in Chinese with English abstract).
Sun S S and McDonough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[A].In:Saunders A D,Norry M J,eds.Magmatism in Oceanic Basins[C].Special Publications.Geologiacl Society London.42:313-345.
Sylvester P J.1989.Post-collisional alkaline granites[J].The Journal of Geology,97(3):261-281.
Sylvester P J.1998.Post-collisional strongly peraluminous granites[J].Lithos,45(1-4):29-44.
Tang G F and Wu S X.1984.Geological research report of the JiaJika granite pegmatite lithium deposit in Kanding County,Sichuan Province[R].Chengdu:Panxi Geological Brigade,Sichuan Geological and Mineral Bureau(in Chinese).
Taylor S R and Mclennan S M.1985.The continental crust:Its composition and evolution[M].Oxford:Blackwel.
Thomas R,Davidson P and Beurlen H.2011a.Tantalite-(Mn)from the Borborema Pegmatite Province,northeastern Brazil:Conditions of formation and melt-and fluid-inclusion constraints on experimental studies[J].Mineralium Deposita,46(7):749-759.
Thomas R,Davidson P and Schmidt C.2011b.Extreme alkali bicarbonate-and carbonate-rich fluid inclusions in granite pegmatite from the Precambrian R?nne granite,Bornholm Island,Denmark[J].Contributions to Mineralogy and Petrology,161(2):315-329
Whalen J B,Currie K L and Chappell B W.1987.A-type granites:Geochemical characteristics,discrimination and petrogenesis[J].Contributions to Mineralogy and Petrology,95(4):407-419.
wang D H,Zou T R,Xu Z G,Yu J J and Fu X F.2004.Advance in the study of using pegmatite deposits as the tracer of orogenic process[J].Advances in Earth Science,19(4):614-620(in Chinese with English abstract).
Wang D H,Li J K and Fu X F.2005.40Ar/39Ar dating for the Jiajika pegmatite-type rare metal deposit in western Sichuan and its significance[J].Geochimica,34(6):541-547(in Chinese with English abstract).
Weislogel A L.2008.Tectonostratigraphic and geochronologic constraints on evolution of the northeast Paleotethys from the Songpan-Ganzi complex,central China[J].Tectonophysics,451(1):331-345.
Wilson M.1989.Igneous petrogenesis[M].London:Allen and Unwin.
Wu F Y,Li X H,Yang J H and Zheng Y F.2007a.Discussions on the petrogenesis of granites[J].Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract).
Wu F Y,Li X H,Yang J H,Zheng Y F and Gao S.2007b.Lu-Hf isotopic systematics and their applications in petrology[J].Acta Petrologica Sinica,23(2):185-220(in Chinese with English abstract).
Wu F Y,Liu Z C,Liu X C and Ji W Q.2015.Himalayan leucogranite:Petrogenesis and implications to orogenesis and plateau uplift[J].Acta Petrologica Sinica,31(1):1-36(in Chinese with English abstract).
Wu F Y,Liu X C,Ji W Q,Wang J M and Yang L.2017.Highly fractionated granites:Recognition and research[J].Science China Earth Sciences,47(7):745-765(in Chinese).
Xiao L,Zhang H F,Clemens J D,Wang Q W,Kan Z Z,Wang K M,Ni PZ and Liu X M.2007.Late Triassic granitoids of the eastern margin of the Tibetan Plateau:Geochronology,petrogenesis and implications for tectonic evolution[J].Lithos,96(3):436-452.
Xu Y F,Qin Y L,Wang X F,Li M Z,Zhou X,Zhan H Y and Wu W H.2019.Geochemical characteristics and metallogenic geological conditions of pegmatite type lithium polymetallic ore in Rongxuka,Sichuan Province[J].Geological Survey of China,6(1):36-42(in Chinese with English abstract).
Xu Z Q,Hou L W,Wang Z X,Fu X F and Huang M H.1992.Orogenic processes of the Songpan-GarzêOrogenic belt of China[M].Beijing:Geological Publishing House(in Chinese).
Xu Z Q and Ma X X.2015.The Chinese Phanerozoic gneiss domes:Subduction-related type,collision-related type and combination type of subduction-collision[J].Acta Petrologica Sinica,31(12):3509-3523(in Chinese with English abstract).
Xu Z Q,Fu X F,Ma X X,Qi X X,Wu C,Hou L W and Zhao Z B.2016.The gneiss domes in Tibetan Plateau and their potential for prospecting[J].Acta Geologica Sinica,90(11):2971-2981(in Chinese with English abstract).
Xu Z Q,Wang R C,Zhao Z B and Fu X F.2018.On the structural backgrounds of the large-scale"Hard-rock type"lithium ore belts in China[J].Acta Geologica Sinica,92(6):1091-1106(in Chinese with English abstract).
Yu J J,Zeng L S,Liu J,Gao L E and Xie K J.2011.Early Miocene leucogranites in Dinggye area,southern Tibet:Formation mechanism and tectonic implications[J].Acta Petrologica Sinica,27(7):1961-1972(in Chinese with English abstract).
Yuan H L,Wu F Y,Gao S,Liu X M,Xu P and Sun D Y.2003.Zircon laser probe U-Pb dating and REE analysis of Cenozoic intrusions in northeast China[J].Chinese Science Bulletin,48(14):1511-1520(in Chinese).
Yuan H L,Gao S,Dai M N,Zong C L,Detlef G,Fontaine G H,Liu XM and Diwu C R.2008.Simultaneous determinations of U-Pb age,Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICP-MS[J].Chemical Geology,247(1-2):100-118.
Yuan J,Xiao L,Wan C H and Gao R.2011.Petrogenesis of Fangmaping-Sanyanlong granites in southern Songpan-Garzêfold belt and its tectonic implication[J].Acta Geologica Sinica,85(2):195-206(in Chinese with English abstract).
Yue X Y,Zhou X,Zhang Y,Gong D X,Zhou Y and Luo L P.2018.Discovery of the pegmatite lithium veins with predicted super-large size resources in the Sizemuzu district of the Keeryin,China[J].China Geology,1(2):310-311.
Zeng L S and Gao L E.2017.Cenozoic crustal anatexis and the leucogranites in the Himalayan collisional orogenic belt[J].Acta Petrologica Sinica,33(5):1420-1444(in Chinese with English abstract).
Zhang H F,Nigel H,Randall P,Zhang L,Zhao Z D and Li D W.2005.Geochemistry of North Himalayan leucogranites:Regional comparison,petrogenesis and tectonic implications[J].Earth ScienceJournal of China University of Geosciences,30(3):275-288(in Chinese with English abstract).
Zhao Y J,Yuan C,Zhou M F,Yan D P,Long X P and Li J L.2007.Geochemistry and petrogenesis of Laojungou and Mengtonggou granites in western Sichuan,China:Constraints on the nature of Songpan-Ganzi basement[J].Acta Petrologica Sinica,23(5):995-1006(in Chinese with English abstract).
Zhou X,Zhou Y,Luo L P,Zhang Y,Xu Y F and Ye Y K.2018.Zircon LA-ICP-MS U-Pb dating of quartz diorite of Rongxuka lithium deposit in western Sichuan and its tectonic implication[J].Journal of Mineralogy and Petrology,38(4):88-97(in Chinese with English abstract).
Zhou Y,Jia Z Q,Zhou X,Zhang Y,Liang B,Yue X Y and Gong D X.2017a.Preliminary analysis of the prospecting law of the Long March Dome in Songpan Ganzi orogenic belt[J].Acta Mineralogica Sinica,37(S):288(in Chinese).
Zhou Y and Zhou X.2017b.The discovery of a large-sized potential rubidium and beryllium deposit in Yazhong area,Daofu County,Sichuan Province[J].News Letters of China Geological Survey,3(21):35-38(in Chinese).
Zhou Y,Zhou X and Zhang Y.2018.Discovery rubidium and beryllium deposit in the Yazhong area of western Sichuan and characteristics of its inclusions,China[A].In Asian Current Research on fluid inclusionsⅦAbstract Volume[C].Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences.165-166.
付小方,侯立玮,王登红,袁蔺平,梁斌,郝雪峰,潘蒙.2014.四川甘孜甲基卡锂辉石矿矿产调查评价成果[J].中国地质调查,1(3):37-43.
付小方,袁蔺平,王登红,侯立玮,潘蒙,郝雪峰,梁斌,唐屹.2015.四川甲基卡矿田新三号稀有金属矿脉的成矿特征与勘查模型[J].矿床地质,34(6):1172-1186.
高利娥,曾令森,侯可军,郭春丽,唐索寒,谢克家,胡古月,王莉.2013.藏南马拉山穹窿佩枯错复合淡色花岗岩体的多期深熔作用[J].科学通报,58(27):2810-2822.
郭素淑,李曙光.2007.淡色花岗岩的岩石学和地球化学特征及其成因[J].地学前缘,14(6):290-298.
古城会.2014.四川省可尔因伟晶岩田东南密集区锂辉石矿床成矿规律[J].地质找矿论丛,29(1):59-65.
郝雪峰,付小方,梁斌,袁蔺平,潘蒙,唐屹.2015.川西甲基卡花岗岩和新三号矿脉的形成时代及意义[J].矿床地质,34(6):1199-1208.
侯立玮,付小方.2002.松潘-甘孜造山带东缘穹隆状变质地质体[M].成都:四川大学出版社.
胡古月,曾令森,陈翰,高利娥.2016.喜马拉雅造山带晚中新世麻迦淡色花岗岩的构建机制[J].地质学报,90(8):1737-1754.
黄春梅,赵志丹,朱弟成,刘栋,黄玉,董铭淳,胡兆初,郑建平.2013.藏南洛扎地区淡色花岗岩锆石U-Pb年龄、Hf同位素、地球化学与岩石成因[J].岩石学报,29(11):3689-3702.
胡健民,孟庆任,石玉若,渠洪杰.2005.松潘-甘孜地体内花岗岩锆石SHRIMPU-Pb定年及其构造意义[J].岩石学报,21(3):867-880.
李建康,王登红,张德会,付小方.2006.四川甲基卡伟晶岩型锂多金属矿床成矿流体来源研究[J].岩石矿物学杂志,25(1):45-52.
梁斌,付小方,唐屹,潘蒙,袁蔺平,郝雪峰.2016.川西甲基卡稀有金属矿区花岗岩岩石地球化学特征[J].桂林理工大学学报,36(1):42-49.
刘丽君,王登红,侯可军,田世洪,赵悦,付小方,袁蔺平,郝雪峰.2017.锂同位素在四川甲基卡新三号矿脉研究中的应用[J].地学前缘,24(5):167-171.
刘应冬,周玉,郭润平,周雄,张贻.2018.四川甲基卡锂辉石矿床西缘地面高精度磁测异常特征及找矿预测[J].矿产勘查,9(3):428-437.
饶魁元.2016.四川马尔康地拉秋锂矿床地质特征及找矿方向[J].四川有色金属,25(1):54-57.
苏嫒娜,田世洪,侯增谦,李建康,李真真,侯可军,李延河,胡文洁,杨竹森.2011.锂同位素及其在四川甲基卡伟晶岩型锂多金属矿床研究中的应用[J].现代地质,25(2):236-242.
唐国凡,吴盛先.1984.四川省康定县甲基卡花岗伟晶岩锂矿床地质研究报告[R].成都:四川地质矿产局攀西地质大队.
王登红,邹天人,徐志刚,余金杰,付小方.2004.伟晶岩矿床示踪造山过程的研究进展[J].地球科学进展,19(4):614-620.
王登红,李建康,付小方.2005.四川甲基卡伟晶岩型稀有金属矿床的成矿时代及其意义[J].地球化学,34(6):541-547.
吴福元,李献华,杨进辉,郑永飞.2007a.花岗岩成因研究的若干问题[J].岩石学报,23(6):1217-1238.
吴福元,李献华,郑永飞,高山.2007b.Lu-Hf同位素体系及其岩石学应用[J].岩石学报,23(2):185-220.
吴福元,刘志超,刘小驰,纪伟强.2015.喜马拉雅淡色花岗岩[J].岩石学报,31(1):1-36.
吴福元,刘小驰,纪伟强,王佳敏,杨雷.2017.高分异花岗岩的识别与研究[J].中国科学:地球科学,47(7):745-765.
徐云峰,秦宇龙,王显锋,李明则,周雄,詹涵钰,武文辉.2019.四川容须卡伟晶岩型锂多金属矿床地球化学特征及成矿地质条件[J].中国地质调查,6(1):36-42.
许志琴,侯立玮,王宗秀,付小方,黄明华.1992.中国松潘-甘孜造山带的造山过程[M].北京：地质出版社.
许志琴,马绪宣.2015.中国大陆显生宙俯冲型、碰撞型和复合型片麻岩穹窿(群)[J].岩石学报,31(12):3509-3523.
许志琴,付小方,马绪宣,戚学祥,吴婵,侯立玮,赵中宝.2016.青藏高原片麻岩穹窿与找矿前景[J].地质学报,90(11):2971-2981.
许志琴,王汝成,赵中宝,付小方.2018.试论中国大陆“硬岩型”大型锂矿带的构造背景[J].地质学报,92(6):1091-1106.
于俊杰,曾令森,刘静,高利娥,谢克家.2011.藏南定结地区早中新世淡色花岗岩的形成机制及其构造动力学意义[J].岩石学报,27(7):1961-1972.
袁洪林,吴福元,高山,柳小明,徐平,孙德有.2003.东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析[J].科学通报,48(14):1511-1520.
袁静,肖龙,万传辉,高睿.2011.松潘-甘孜南部放马坪-三岩龙花岗岩的成因及其构造意义[J].地质学报,85(2):195-206.
曾令森,高利娥.2017.喜马拉雅碰撞造山带新生代地壳深熔作用与淡色花岗岩[J].岩石学报,33(5):1420-1444.
张宏飞,Nigel Harris,Randall Parrish,张利,赵志丹,李德威.2005.北喜马拉雅淡色花岗岩地球化学:区域对比、岩石成因及其构造意义[J].地球科学,30(3):275-288.
赵永久,袁超,周美夫,颜丹平,龙晓平,李继亮.2007.川西老君沟和孟通沟花岗岩的地球化学特征、成因机制及对松潘-甘孜地体基底性质的制约[J].岩石学报,23(5):995-1006.
周雄,周玉,罗丽萍,张贻,徐云峰,叶亚康.2018.川西容须卡锂辉石矿床石英闪长岩锆石LA-ICP MS测年及构造意义[J].矿物岩石,38(4):88-97.
周玉,贾志泉,周雄,张贻,梁兵,岳相元,龚大兴.2017a.松潘甘孜造山带长征穹窿找矿规律初析[J].矿物学报,37(S):288.
周玉,周雄.2017b.四川道孚县亚中地区发现具有大型规模潜力铷铍矿[J].中国地质调查成果快讯,3(21):35-38.
Bakker R J and Elburg M A.2006.A magmatic-hydrothermal transition in Arkaroola(northern Flinders Ranges,South Australia):From diopside-titanite pegmatites to hematite-quartz growth[J].Contributions to Mineralogy and Petrology,152(5):541-569.
Barbarin B.1999.A review of the relationships between granitoid types,their origins and their geodynamic environments[J].Lithos,46(3):605-626.
Bau M.1996.Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems:Evidence from Y/Ho,Zr/Hf,and lanthanide tetrad effect[J].Contributions to Mineralogy and Petrology,123(3):323-333.
Boynton W V.1984.Geochemistry of the rare earth elements:Meteoritestudies[A].In:Henderson P,ed.Rare earth element geochemistry[C].Amsterdam:Elsevier.63-114.
Cohen K M,Finney S C,Gibbard P L and Fan J X.2013.The ICSinternational chronostratigraphic chart[J].Episodes,36(3):199-204
Dill H G.2015.Pegmatites and aplites:Their genetic and applied ore geology[J].Ore Geology Reviews,69:417-561.
Fu X F,Hou L W,Wang D H,Yuan L P,Liang B,Hao X F and Pan M.2014.Achievements in the investigation and evaluation of Spodumene resources at Jiajika in Sichuan,China[J].Geological Survey of China,1(3):37-43(in Chinese with English abstract).
Fu X F,Yuan L P,Wang D H,Hou L W,Pan M,Hao X F,Liang B and Tang Y.2015.Mineralization characteristics and prospecting model of newly discovered X03 rare metal vein in Jiajika orefield,Sichuan[J].Mineral Deposits,34(6):1172-1186(in Chinese with English abstract).
Gao L E,Zeng L S,Hou K J,Guo C L,Tang S H,Xie K J,Hu G Y and Wang L.2013.Episodic crustal anatexis and the formation of Paiku composite leucogranitic pluton in the Malashan gneiss dome,southern Tibet[J].Chinese Science Bulletin,58(27):2810-2822(in Chinese with English abstract).
Guo S S and Li S G.2007.Petrological and geochemical constraints on the origin of leucogranites[J].Earth Science Frontiers,14(6):290-298(in Chinese with English abstract).
Gu C H.2014.Metallogenic regularity of spodumene deposits in the closely spaced pegmatite area in the southeastern Keeryin pegmatite field,Sichuan Province[J].Contributions to Geology and Mineral Resources Research,29(1):59-65(in Chinese with English abstract).
Hao X F,Fu X F,Liang B,Yuan L P,Pan M and Tang Y.2015.Formation ages of granite and X03 pegmatite vein in Jiajika,western Sichuan,and their geological significance[J].Mineral Deposits,34(6):1199-1208(in Chinese with English abstract).
Harris N B W and Inger S.1992.Trace element modelling of pelite-derived granites:Contributions to mineralogy and petrology[J].Contributions to Mineralogy and Petrology,110(1):46-56.
Hou L W and Fu X F.2002.Dome-shaped metamorphic geological body on the eastern margin of Songpan-Ganzi orogenic belt[M].Sichuan University Press(in Chinese).
Hu G Y,Zeng L S,Chen H and Gao L E.2016.Assembling mechanism for the Late-Miocene Mabja leucogranite pluton,Himalayan Orogen[J].Acta Geologica Sinica,90(8):1737-1754(in Chinese with English abstract).
Huang C M,Zhao Z D,Zhu D C,Liu D,Huang Y,Dong M C,Hu Z Cand Zheng J P.2013.Geochemistry,zircon U-Pb chronology and Hf isotope of Luozha leucogranite,southern Tibet:Implication for petrogenesis[J].Acta Petrologica Sinica,29(11):3689-3702(in Chinese with English abstract).
Hu J M,Meng Q R,Shi Y R and Qu H J.2005.SHRIMP U-Pb dating of zircons from granitoid bodies in the Songpan-Ganzi terrane and its implications[J].Acta Petrologica Sinica,21(3):867-880(in Chinese with English abstract).
Le Fort P.1973.Les leucogranitesàtourmaline de l’Himalaya sur l’exemple du granite du Manaslu(Népal central)[J].Bulletin de la Societe Geologique de France,15(5-6):555-561(in France).
Le Maitre R W.1989.A classification of igneous rocks and glossary of terms[M].Oxford:Black Well.
Li J K,Wang D H,Zhang D H and Fu X F.2006.The source of oreforming fluid in Jiajika pegmatite type lithium polymetallic deposit,Sichuan Province[J].Acta Petrologica et Mineralogica,25(1):45-52(in Chinese with English abstract).
Li X H,Li Z X,Li W X,Liu Y,Yuan C,Wei G J and Qi C S.2007.U-Pb zircon,geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I-and A-type granites from central Guangdong,SE China:A major igneous event in response to foundering of a subducted flat-slab[J]?Lithos,96(1):186-204.
Liang B,Fu X F,Tang Y,Pan M,Yuan L P and Hao X F.2016.Granite geochemical characteristics in Jiajika rare metal deposit,western Sichuan[J].Journal of Guilin University of Technology,36(1):42-49(in Chinese with English abstract).
Liu L J,Wang D H,Hou K J,Tian S H,Zhao Y,Fu X F,Yuan L P and Hao X F.2017.Application of lithium isotope to Jiajika new No.3pegmatite lithium polymetallic vein in Sichuan[J].Earth Science Frontiers,24(5):167-171(in Chinese with English abstract).
Liu Y D,Zhou Y,Guo R P,Zhou X and Zhang Y.2018.Anomalies characteristics of ground high-precision magnetic survey and the prospecting prediction in Jiajika style spodumene deposits,Sichuan[J].Mineral Exploration,9(3):428-437(in Chinese with English abstract).
London D and Morgan G B.2012.The pegmatite puzzle[J].Elements,8(4):263-268.
London D.2014.A petrologic assessment of internal zonation in granitic pegmatites[J].Lithos,184-187(1):74-104.
Ludwig K R.2003.Isoplot 3.0-A geochronological toolkit for Microsoft Excel.Berkeley geochronology center[M].Special Publication.(4):1-70.
Maniar P D and Piccoli P M.1989.Tectonic discrimination of granitoids[J].Geological Society of America Bulletin,101(5):635-643
Pati?o Douce A E and Harris N.1998.Experimental constraints on Himalayan anatexis[J].Journal of Petrology,39(4):689-710.
Pearce J A and Mei H.1988.Volcanic rocks of the 1985 Tibet Geotraverse:Lhasa to Golmud[J].Philosophical Transactions of the Royal Society of London,327(1594):169-201.
Pearce J A.1996.Sources and settings of granitic rocks[J].Episodes,19(4):120-125.
Rao K Y.2016.The geological characteristics and ore exploration targeting of Dilaqiu Lithium deposit in Maerkang County,Sichuan Provice[J].Sichuan Nonferrous Metals,25(1):54-57(in Chinese with English abstract).
Roger F,Calassou S,Lancelot J,Malavieille J,Mattauer M,Xu Z Q,Hao Z W and Hou L W.1995.Miocene emplacement and deformation of the Konga Shan granite(Xianshui He fault zone,West Sichuan,China):Geodynamic implications[J].Earth and Planetary Science Letters,130(1-4):201-216.
Roger F,Malavieille J,Leloup P H,Calassou S and Xu Z.2004.Timing of granite emplacement and cooling in the Songpan-GarzêFold Belt(eastern Tibetan Plateau)with tectonic implications[J].Journal of Asian Earth Sciences,22(5):465-481.
Roger F,Jolivet M and Malavieille J.2010.The tectonic evolution of the Songpan-Garzê(North Tibet)and adjacent areas from Proterozoic to Present:A synthesis[J].Journal of Asian Earth Sciences,39(4):254-269.
Rollinson H R.1993.Using geochemical date:Evaluation,presentation and interpretation[M].New York:Longman Group UK Ltd.
Su A N,Tian S H,Hou Z Q,Li J K,Li Z Z,Hou K J,Li Y H,Hu W Jand Yuan Z S.2011.Lithium isotope and its application to Jiajika pegmatite type lithium polymetallic deposit in Sichuan[J].Geoscience,25(2):236-242(in Chinese with English abstract).
Sun S S and McDonough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[A].In:Saunders A D,Norry M J,eds.Magmatism in Oceanic Basins[C].Special Publications.Geologiacl Society London.42:313-345.
Sylvester P J.1989.Post-collisional alkaline granites[J].The Journal of Geology,97(3):261-281.
Sylvester P J.1998.Post-collisional strongly peraluminous granites[J].Lithos,45(1-4):29-44.
Tang G F and Wu S X.1984.Geological research report of the JiaJika granite pegmatite lithium deposit in Kanding County,Sichuan Province[R].Chengdu:Panxi Geological Brigade,Sichuan Geological and Mineral Bureau(in Chinese).
Taylor S R and Mclennan S M.1985.The continental crust:Its composition and evolution[M].Oxford:Blackwel.
Thomas R,Davidson P and Beurlen H.2011a.Tantalite-(Mn)from the Borborema Pegmatite Province,northeastern Brazil:Conditions of formation and melt-and fluid-inclusion constraints on experimental studies[J].Mineralium Deposita,46(7):749-759.
Thomas R,Davidson P and Schmidt C.2011b.Extreme alkali bicarbonate-and carbonate-rich fluid inclusions in granite pegmatite from the Precambrian R?nne granite,Bornholm Island,Denmark[J].Contributions to Mineralogy and Petrology,161(2):315-329
Whalen J B,Currie K L and Chappell B W.1987.A-type granites:Geochemical characteristics,discrimination and petrogenesis[J].Contributions to Mineralogy and Petrology,95(4):407-419.
wang D H,Zou T R,Xu Z G,Yu J J and Fu X F.2004.Advance in the study of using pegmatite deposits as the tracer of orogenic process[J].Advances in Earth Science,19(4):614-620(in Chinese with English abstract).
Wang D H,Li J K and Fu X F.2005.40Ar/39Ar dating for the Jiajika pegmatite-type rare metal deposit in western Sichuan and its significance[J].Geochimica,34(6):541-547(in Chinese with English abstract).
Weislogel A L.2008.Tectonostratigraphic and geochronologic constraints on evolution of the northeast Paleotethys from the Songpan-Ganzi complex,central China[J].Tectonophysics,451(1):331-345.
Wilson M.1989.Igneous petrogenesis[M].London:Allen and Unwin.
Wu F Y,Li X H,Yang J H and Zheng Y F.2007a.Discussions on the petrogenesis of granites[J].Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract).
Wu F Y,Li X H,Yang J H,Zheng Y F and Gao S.2007b.Lu-Hf isotopic systematics and their applications in petrology[J].Acta Petrologica Sinica,23(2):185-220(in Chinese with English abstract).
Wu F Y,Liu Z C,Liu X C and Ji W Q.2015.Himalayan leucogranite:Petrogenesis and implications to orogenesis and plateau uplift[J].Acta Petrologica Sinica,31(1):1-36(in Chinese with English abstract).
Wu F Y,Liu X C,Ji W Q,Wang J M and Yang L.2017.Highly fractionated granites:Recognition and research[J].Science China Earth Sciences,47(7):745-765(in Chinese).
Xiao L,Zhang H F,Clemens J D,Wang Q W,Kan Z Z,Wang K M,Ni PZ and Liu X M.2007.Late Triassic granitoids of the eastern margin of the Tibetan Plateau:Geochronology,petrogenesis and implications for tectonic evolution[J].Lithos,96(3):436-452.
Xu Y F,Qin Y L,Wang X F,Li M Z,Zhou X,Zhan H Y and Wu W H.2019.Geochemical characteristics and metallogenic geological conditions of pegmatite type lithium polymetallic ore in Rongxuka,Sichuan Province[J].Geological Survey of China,6(1):36-42(in Chinese with English abstract).
Xu Z Q,Hou L W,Wang Z X,Fu X F and Huang M H.1992.Orogenic processes of the Songpan-GarzêOrogenic belt of China[M].Beijing:Geological Publishing House(in Chinese).
Xu Z Q and Ma X X.2015.The Chinese Phanerozoic gneiss domes:Subduction-related type,collision-related type and combination type of subduction-collision[J].Acta Petrologica Sinica,31(12):3509-3523(in Chinese with English abstract).
Xu Z Q,Fu X F,Ma X X,Qi X X,Wu C,Hou L W and Zhao Z B.2016.The gneiss domes in Tibetan Plateau and their potential for prospecting[J].Acta Geologica Sinica,90(11):2971-2981(in Chinese with English abstract).
Xu Z Q,Wang R C,Zhao Z B and Fu X F.2018.On the structural backgrounds of the large-scale"Hard-rock type"lithium ore belts in China[J].Acta Geologica Sinica,92(6):1091-1106(in Chinese with English abstract).
Yu J J,Zeng L S,Liu J,Gao L E and Xie K J.2011.Early Miocene leucogranites in Dinggye area,southern Tibet:Formation mechanism and tectonic implications[J].Acta Petrologica Sinica,27(7):1961-1972(in Chinese with English abstract).
Yuan H L,Wu F Y,Gao S,Liu X M,Xu P and Sun D Y.2003.Zircon laser probe U-Pb dating and REE analysis of Cenozoic intrusions in northeast China[J].Chinese Science Bulletin,48(14):1511-1520(in Chinese).
Yuan H L,Gao S,Dai M N,Zong C L,Detlef G,Fontaine G H,Liu XM and Diwu C R.2008.Simultaneous determinations of U-Pb age,Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICP-MS[J].Chemical Geology,247(1-2):100-118.
Yuan J,Xiao L,Wan C H and Gao R.2011.Petrogenesis of Fangmaping-Sanyanlong granites in southern Songpan-Garzêfold belt and its tectonic implication[J].Acta Geologica Sinica,85(2):195-206(in Chinese with English abstract).
Yue X Y,Zhou X,Zhang Y,Gong D X,Zhou Y and Luo L P.2018.Discovery of the pegmatite lithium veins with predicted super-large size resources in the Sizemuzu district of the Keeryin,China[J].China Geology,1(2):310-311.
Zeng L S and Gao L E.2017.Cenozoic crustal anatexis and the leucogranites in the Himalayan collisional orogenic belt[J].Acta Petrologica Sinica,33(5):1420-1444(in Chinese with English abstract).
Zhang H F,Nigel H,Randall P,Zhang L,Zhao Z D and Li D W.2005.Geochemistry of North Himalayan leucogranites:Regional comparison,petrogenesis and tectonic implications[J].Earth ScienceJournal of China University of Geosciences,30(3):275-288(in Chinese with English abstract).
Zhao Y J,Yuan C,Zhou M F,Yan D P,Long X P and Li J L.2007.Geochemistry and petrogenesis of Laojungou and Mengtonggou granites in western Sichuan,China:Constraints on the nature of Songpan-Ganzi basement[J].Acta Petrologica Sinica,23(5):995-1006(in Chinese with English abstract).
Zhou X,Zhou Y,Luo L P,Zhang Y,Xu Y F and Ye Y K.2018.Zircon LA-ICP-MS U-Pb dating of quartz diorite of Rongxuka lithium deposit in western Sichuan and its tectonic implication[J].Journal of Mineralogy and Petrology,38(4):88-97(in Chinese with English abstract).
Zhou Y,Jia Z Q,Zhou X,Zhang Y,Liang B,Yue X Y and Gong D X.2017a.Preliminary analysis of the prospecting law of the Long March Dome in Songpan Ganzi orogenic belt[J].Acta Mineralogica Sinica,37(S):288(in Chinese).
Zhou Y and Zhou X.2017b.The discovery of a large-sized potential rubidium and beryllium deposit in Yazhong area,Daofu County,Sichuan Province[J].News Letters of China Geological Survey,3(21):35-38(in Chinese).
Zhou Y,Zhou X and Zhang Y.2018.Discovery rubidium and beryllium deposit in the Yazhong area of western Sichuan and characteristics of its inclusions,China[A].In Asian Current Research on fluid inclusionsⅦAbstract Volume[C].Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences.165-166.
付小方,侯立玮,王登红,袁蔺平,梁斌,郝雪峰,潘蒙.2014.四川甘孜甲基卡锂辉石矿矿产调查评价成果[J].中国地质调查,1(3):37-43.
付小方,袁蔺平,王登红,侯立玮,潘蒙,郝雪峰,梁斌,唐屹.2015.四川甲基卡矿田新三号稀有金属矿脉的成矿特征与勘查模型[J].矿床地质,34(6):1172-1186.
高利娥,曾令森,侯可军,郭春丽,唐索寒,谢克家,胡古月,王莉.2013.藏南马拉山穹窿佩枯错复合淡色花岗岩体的多期深熔作用[J].科学通报,58(27):2810-2822.
郭素淑,李曙光.2007.淡色花岗岩的岩石学和地球化学特征及其成因[J].地学前缘,14(6):290-298.
古城会.2014.四川省可尔因伟晶岩田东南密集区锂辉石矿床成矿规律[J].地质找矿论丛,29(1):59-65.
郝雪峰,付小方,梁斌,袁蔺平,潘蒙,唐屹.2015.川西甲基卡花岗岩和新三号矿脉的形成时代及意义[J].矿床地质,34(6):1199-1208.
侯立玮,付小方.2002.松潘-甘孜造山带东缘穹隆状变质地质体[M].成都:四川大学出版社.
胡古月,曾令森,陈翰,高利娥.2016.喜马拉雅造山带晚中新世麻迦淡色花岗岩的构建机制[J].地质学报,90(8):1737-1754.
黄春梅,赵志丹,朱弟成,刘栋,黄玉,董铭淳,胡兆初,郑建平.2013.藏南洛扎地区淡色花岗岩锆石U-Pb年龄、Hf同位素、地球化学与岩石成因[J].岩石学报,29(11):3689-3702.
胡健民,孟庆任,石玉若,渠洪杰.2005.松潘-甘孜地体内花岗岩锆石SHRIMPU-Pb定年及其构造意义[J].岩石学报,21(3):867-880.
李建康,王登红,张德会,付小方.2006.四川甲基卡伟晶岩型锂多金属矿床成矿流体来源研究[J].岩石矿物学杂志,25(1):45-52.
梁斌,付小方,唐屹,潘蒙,袁蔺平,郝雪峰.2016.川西甲基卡稀有金属矿区花岗岩岩石地球化学特征[J].桂林理工大学学报,36(1):42-49.
刘丽君,王登红,侯可军,田世洪,赵悦,付小方,袁蔺平,郝雪峰.2017.锂同位素在四川甲基卡新三号矿脉研究中的应用[J].地学前缘,24(5):167-171.
刘应冬,周玉,郭润平,周雄,张贻.2018.四川甲基卡锂辉石矿床西缘地面高精度磁测异常特征及找矿预测[J].矿产勘查,9(3):428-437.
饶魁元.2016.四川马尔康地拉秋锂矿床地质特征及找矿方向[J].四川有色金属,25(1):54-57.
苏嫒娜,田世洪,侯增谦,李建康,李真真,侯可军,李延河,胡文洁,杨竹森.2011.锂同位素及其在四川甲基卡伟晶岩型锂多金属矿床研究中的应用[J].现代地质,25(2):236-242.
唐国凡,吴盛先.1984.四川省康定县甲基卡花岗伟晶岩锂矿床地质研究报告[R].成都:四川地质矿产局攀西地质大队.
王登红,邹天人,徐志刚,余金杰,付小方.2004.伟晶岩矿床示踪造山过程的研究进展[J].地球科学进展,19(4):614-620.
王登红,李建康,付小方.2005.四川甲基卡伟晶岩型稀有金属矿床的成矿时代及其意义[J].地球化学,34(6):541-547.
吴福元,李献华,杨进辉,郑永飞.2007a.花岗岩成因研究的若干问题[J].岩石学报,23(6):1217-1238.
吴福元,李献华,郑永飞,高山.2007b.Lu-Hf同位素体系及其岩石学应用[J].岩石学报,23(2):185-220.
吴福元,刘志超,刘小驰,纪伟强.2015.喜马拉雅淡色花岗岩[J].岩石学报,31(1):1-36.
吴福元,刘小驰,纪伟强,王佳敏,杨雷.2017.高分异花岗岩的识别与研究[J].中国科学:地球科学,47(7):745-765.
徐云峰,秦宇龙,王显锋,李明则,周雄,詹涵钰,武文辉.2019.四川容须卡伟晶岩型锂多金属矿床地球化学特征及成矿地质条件[J].中国地质调查,6(1):36-42.
许志琴,侯立玮,王宗秀,付小方,黄明华.1992.中国松潘-甘孜造山带的造山过程[M].北京：地质出版社.
许志琴,马绪宣.2015.中国大陆显生宙俯冲型、碰撞型和复合型片麻岩穹窿(群)[J].岩石学报,31(12):3509-3523.
许志琴,付小方,马绪宣,戚学祥,吴婵,侯立玮,赵中宝.2016.青藏高原片麻岩穹窿与找矿前景[J].地质学报,90(11):2971-2981.
许志琴,王汝成,赵中宝,付小方.2018.试论中国大陆“硬岩型”大型锂矿带的构造背景[J].地质学报,92(6):1091-1106.
于俊杰,曾令森,刘静,高利娥,谢克家.2011.藏南定结地区早中新世淡色花岗岩的形成机制及其构造动力学意义[J].岩石学报,27(7):1961-1972.
袁洪林,吴福元,高山,柳小明,徐平,孙德有.2003.东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析[J].科学通报,48(14):1511-1520.
袁静,肖龙,万传辉,高睿.2011.松潘-甘孜南部放马坪-三岩龙花岗岩的成因及其构造意义[J].地质学报,85(2):195-206.
曾令森,高利娥.2017.喜马拉雅碰撞造山带新生代地壳深熔作用与淡色花岗岩[J].岩石学报,33(5):1420-1444.
张宏飞,Nigel Harris,Randall Parrish,张利,赵志丹,李德威.2005.北喜马拉雅淡色花岗岩地球化学:区域对比、岩石成因及其构造意义[J].地球科学,30(3):275-288.
赵永久,袁超,周美夫,颜丹平,龙晓平,李继亮.2007.川西老君沟和孟通沟花岗岩的地球化学特征、成因机制及对松潘-甘孜地体基底性质的制约[J].岩石学报,23(5):995-1006.
周雄,周玉,罗丽萍,张贻,徐云峰,叶亚康.2018.川西容须卡锂辉石矿床石英闪长岩锆石LA-ICP MS测年及构造意义[J].矿物岩石,38(4):88-97.
周玉,贾志泉,周雄,张贻,梁兵,岳相元,龚大兴.2017a.松潘甘孜造山带长征穹窿找矿规律初析[J].矿物学报,37(S):288.
周玉,周雄.2017b.四川道孚县亚中地区发现具有大型规模潜力铷铍矿[J].中国地质调查成果快讯,3(21):35-38.
© 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 |