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塔里木陆块西北缘萨热克砂岩型铜矿床构造-流体演化对成矿的制约
引用本文:王伟,李文渊,高满新,熊中乙,李天虎,宿晓虹,郭周平,孟勇,全守村,刘增仁,叶雷,陈传庆,唐小东.塔里木陆块西北缘萨热克砂岩型铜矿床构造-流体演化对成矿的制约[J].地质通报,2018,37(7):1315-1324.
作者姓名:王伟  李文渊  高满新  熊中乙  李天虎  宿晓虹  郭周平  孟勇  全守村  刘增仁  叶雷  陈传庆  唐小东
作者单位:长安大学地球科学与资源学院;国土资源部岩浆作用成矿与找矿重点实验室/中国地质调查局西安地质调查中心;有色金属矿产地质调查中心新疆地质调查所;中国冶金地质勘查工程总局新疆地质勘查院
基金项目:中国地质调查局项目《天山-北山成矿带那拉提-营毛沱地区地质矿产调查》(编号:DD20160009)、《西昆仑铁铅锌资源基地调查与勘查示范》(编号:DD20160015)和《新疆西南天山萨瓦甫齐地区矿产地质调查》(编号:12120113043700)
摘    要:塔里木陆块西北缘萨热克砂岩型铜矿床构造演化、流体演化与成矿之间具有密切关系,处于一个统一系统中。矿床成岩期方解石中包裹体水的δD值为-65.3‰~-99.2‰,改造成矿期石英包裹体水的δD值为-77.7‰~-96.3‰,成岩成矿期成矿流体δ~(18)OH_2O变化范围为-3.22‰~1.84‰,改造成矿期成矿流体δ~(18)OH_2O变化范围为-4.26‰~5.14‰,指示萨热克铜矿成岩期、改造期成矿流体主要为中生代大气降水及其经水岩作用而成的盆地卤水。矿石中辉铜矿δ~(34)S值为-24.7‰~-15.4‰,指示硫主要源自硫酸盐细菌与有机质还原,部分源于有机硫。构造与成矿流体演化对砂岩铜矿成矿起关键制约作用。盆地发展早期强烈的抬升运动使盆地周缘基底与古生界剥蚀,为富铜矿源层的形成提供了丰富物源,至晚侏罗世盆地发展晚期,长期演化积聚的巨量含矿流体在库孜贡苏组砾岩胶结物及裂隙中富集,在萨热克巴依盆地内形成具有经济意义的砂岩型铜矿床。

关 键 词:塔里木陆块  萨热克  砂岩型铜矿  构造  流体  成矿体系
收稿时间:2017/12/15 0:00:00
修稿时间:2018/3/20 0:00:00

Constraints on tectonic, fluid and metallogenic system evolution for the formation of Sareke sandstone copper deposit in northwestern Tarim block
WANG Wei,LI Wenyuan,GAO Manxin,XIONG Zhongyi,LI Tianhu,SU Xiaohong,GUO Zhouping,MENG Yong,QUAN Shoucun,LIU Zengren,YE Lei,CHEN Chuanqing and TANG Xiaodong.Constraints on tectonic, fluid and metallogenic system evolution for the formation of Sareke sandstone copper deposit in northwestern Tarim block[J].Geologcal Bulletin OF China,2018,37(7):1315-1324.
Authors:WANG Wei  LI Wenyuan  GAO Manxin  XIONG Zhongyi  LI Tianhu  SU Xiaohong  GUO Zhouping  MENG Yong  QUAN Shoucun  LIU Zengren  YE Lei  CHEN Chuanqing and TANG Xiaodong
Institution:Faculty of Earth Science and Resources, Chang''an University, Xi''an 710054, Shaanxi, China;Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Faculty of Earth Science and Resources, Chang''an University, Xi''an 710054, Shaanxi, China;Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MLR/Xi''an Center of Geological Survey, CGS, Xi''an 710054, Shaanxi, China,Xinjiang Geological Survey Institute of China Non-ferrrous Metals Resource Geological Survey, Urumqi 830011, Xinjiang, China,Xinjiang Geological Survey Institute of China Non-ferrrous Metals Resource Geological Survey, Urumqi 830011, Xinjiang, China,Xinjiang Institute of China Geological Exploration and Engineering Bureau, Urumqi 830000, Xinjiang, China and Xinjiang Institute of China Geological Exploration and Engineering Bureau, Urumqi 830000, Xinjiang, China
Abstract:
Keywords:Tarim block  Sareke  sandstone copper deposit  tectonic  fluid  metallogenic system
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