世界地质    2018 37 (2): 399-408   ISSN: 1004-5589  CN: 22-1111/P   西藏双湖地区南措铜金矿区花岗闪长岩锆石U-Pb年代学、岩石地球化学及成因 王启, 孙丰月, 王琳琳, 王力, 张志颖 吉林大学 地球科学学院, 长春 130061 收稿日期 2017-12-15  修回日期 2018-02-21  网络版发布日期 null 参考文献  [1] 史春清,孙丰月,黄维平,等. 西藏那曲南措金铜矿区酸性侵入岩锆石U-Pb年龄、地球化学特征及地质意义[J]. 黄金,2017,38(4):7-15. SHI Chun-qing,SUN Feng-yue,HUANG Wei-ping,et al. Zircon U-Pb ages and geochemical characteristics of the acidic intrusive rocks in Nancuo Au-Cu deposit,Nakchu,Tibet,and its geological significance[J].Gold,2017,38(4):7-15. [2] 惠艳梅,吕鹏,梁玉恩. 西藏双湖特别区南措铜矿特征及成因探讨[J].吉林地质,2012,31(4):36-40. HUI Yan-mei,LYU Peng,LIANG Yu-en.Geological features and genesis of Nancuo copper deposit in Shuanghu special district,Tibet[J].Jilin Geology,2012,31(4):36-40. [3] 尚毅广,孙丰月,姜和芳,等. 大兴安岭北段霍洛台铜铅锌矿区花岗闪长岩的岩石成因:地球化学和锆石U-Pb年代学制约[J].世界地质,2017,36(2):474-485. SHANG Yi-guang,SUN Feng-yue,JIANG He-fang,et al. Petrogenesis of granodiorites in Huoluotai Cu-Pb-Zn mining area:constrain from geochemistry and zircon U-Pb geochronology,northern Daxing'anling[J]. Global Geology,2017,36(2):474-485. [4] 陈红旗,曲晓明,范淑芳. 西藏改则县多龙矿集区斑岩型铜金矿床的地质特征与成矿——找矿模型[J].矿床地质,2015,34(2):321-332. CHEN Hong-qi,QU Xiao-ming,FAN Shu-fang. Geological characteristics and metallogenic prospecting model of Duolong porphyry copper gold ore concentration area in Gerze County,Tibet[J]. Mineral Deposits,2015,34(2):321-332. [5] 史春清. 西藏安多南措金多金属矿床地质特征及矿化富集规律研究:硕士学位论文[D].长春:吉林大学,2017. SHI Chun-qing. Study on the geological characteristics and enrichment regularities of mineralization of Nancuo gold polymetallic deposit in Amdo area,Tibet:master's degree thesis[D]. Changchun:Jilin University,2017. [6] Andersen T,Griffin W L,Pearson N J. Crustal evolution in the SW part of the Baltic Shield:the Hf isotope evidence[J]. Journal of Petrology,2002,43(9):1725-1747. [7] Hoskin P W,Black L P. Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon[J]. Journal of Metamorphic Geology,2000,18(4):423-439. [8] Chappell B W. Aluminum saturation in I-and S-type granites and the characterization of fractionated haplogranites[J].Lithos,1999,46(3):535-551. [9] 纪政,葛文春,杨浩,等.大兴安岭中段塔尔气地区早白垩世花岗岩成因及形成构造环境[J]. 世界地质,2016,35(2):283-296. JI Zheng,GE Wen-chun,YANG Hao,et al. Petrogenesis of Early Cretaceous granites in Taerqi area of central Great Xing'an Range and its tectonic setting[J]. Global Geology,2016,35(2):283-296. [10] Xu W L,Ji W Q,Pei F P,et al.Triassic volcanism in eastern Heilongjiang and Jilin provinces,NE China:chronology,geochemistry,and tectonic implications[J]. Journal of Asian Earth Sciences,2009,34(34):392-402. [11] Weaver B L,Tarney J. Empirical approach to estimating the composition of the continental crust[J]. Nature,1984,310(5978):575-577. [12] Tischendorf G,Paelchen W. On the classification of granitoids[J]. Zeitschrift Fuer Geologische Wissenschaften,1985,13(5):615-627. [13] Kapp P,Murphy M A,Yin A.Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet[J].Tectonics,2003,22(4):3-23. [14] 朱弟成,潘桂棠,莫宣学,等.青藏高原中部中生代OIB型玄武岩的识别:年代学、地球化学及其构造环境[J].地质学报,2006,80(9):1312-1328. ZHU Di-cheng,PAN Gui-tang,MO Xuan-xue,et al. Identification for the Mesozoic OIB-type basalts in Central Qinghai-Tibetan Plateau:geochronology,geochemistry and their tectonic setting[J]. Acta Geologica Sinica,2006,80(9):1312-1328. [15] 潘桂棠,莫宣学,侯增谦,等.冈底斯造山带的时空结构及演化[J].岩石学报,2006,22(3):521-533. PAN Gui-tang,MO Xuan-xue,HOU Zeng-qian,et al. Spatial-temporal framework of the Gangdese Orogenic Belt and its evolution[J]. Acta Petrologica Sinica,2006,22(3):521-533. [16] 李金祥,李光明,秦克章,等.班公湖带多不杂富金斑岩铜矿床斑岩——火山岩的地球化学特征与时代对成矿构造背景的制约[J].岩石学报,2008,24(3):531-543. LI Jin-xiang,LI Guang-ming,QIN Ke-zhang,et al. Geochemistry of porphyries and volcanic rocks and ore-forming geochronology of Duobuza gold-rich porphyry copper deposit in Bangonghu belt,Tibet:constraints on metallogenic tectonic settings[J]. Acta Petrologica Sinica,2008,24(3):531-543. [17] 范建军. 班公湖-怒江洋中西段晚中生代汇聚消亡时空重建:博士学位论文[D].长春:吉林大学,2016. FAN Jian-jun. Reconstructing the Late Mesozoic closing process of the middle and western segments of the Bangong-Nujiang ocean in space and time:doctor's degree thesis[D].Changchun:Jilin University,2016. [18] 史仁灯.西藏班公湖MOR型和SSZ型两套蛇绿岩的厘定及大地构造意义:博士学位论文[D].北京:中国地质科学院,2005. SHI Ren-deng. Recognition of the Bangong Lake MOR-and SSZ-type ophiolites in the northwestern Tibet Plateau and its tectonic significance:doctor's degree thesis[D].Beijing:Chinese Academy of Geological Science,2005. [19] 曲晓明,王瑞江,辛洪波,等.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学[J].地球化学,2009,38(6):523-535. QU Xiao-ming,WANG Rui-jiang,XIN Hong-bo,et al. Geochronology and geochemistry of igneous rock related to the subduction of the Tethys oceanic plate along the Bangong Lake arc zone,the western Tibetan Plateau[J]. Geochimica,2009,38(6):523-535. [20] 许荣科,郑有业,赵平甲,等.西藏东巧北尕苍见岛弧的厘定及地质意义[J].中国地质,2007,34(5):768-777. XU Rong-ke,ZHENG You-ye,ZHAO Ping-jia,et al. Definition and geological significance of the Gacangjian volcanic arc north of Dongqiao,Tibet[J]. Geology in China,2007,34(5):768-777. [21] Richards J P.Tectono-magmatic precursors for porphyry Cu-(Mo-Au) deposit formation[J].Economic Geology,2003,98(8):1515-1533. 通讯作者: 孙丰月(1963-),男,教授,博士生导师,主要从事矿床学的教学与研究工作.E-mail:sfy@jlu.edu.cn