塔西地区中—新生代盆-山-原镶嵌构造区:砂砾岩型铜铅锌-天青石-铀-煤成矿系统
|
摘要
塔里木盆地西部地区(简称"塔西地区")中—新生代盆-山-原镶嵌构造区形成了铜铅锌-天青石-铀-石膏-煤-天然气等多矿种同盆共存富集成藏成矿,是中国陆内特色成矿单元。以成矿系统理论和波浪镶嵌构造理论为指导,采用构造岩相学研究方法,对砂砾岩型铜铅锌-天青石-铀-煤成矿系统的物质-时间-空间结构模型进行研究,探索该陆内特色成矿单元内区域成矿规律。按照塔西地区盆-山-原耦合转换不同期次的构造岩相学序列、构造岩相学组合类型、原型盆地和盆地动力学等综合角度,将塔西地区砂砾岩型铜铅锌-天青石-铀-煤成矿系统划分为燕山期铜多金属-铀-煤成矿亚系统、燕山晚期—喜山早期铅锌-天青石-铀成矿亚系统、喜山晚期铜-铀成矿亚系统。它们在物质-时间-空间分布规律上受塔西地区盆-山-原镶嵌构造区挤压-伸展转换过程控制显著。燕山期铜多金属-铀-煤成矿亚系统形成于中生代陆内走滑拉分断陷盆地中,受对冲式厚皮型逆冲推覆构造系统、裙边式复式向斜构造和碱性辉长辉绿岩脉群侵入构造系统等复合控制,形成于盆地正反转构造期并耦合了深部热正反转构造作用。燕山晚期—喜山早期铅锌-天青石-铀成矿亚系统分布在乌拉根晚白垩世—古近纪挤压-伸展转换盆地中,受后展式厚皮型前陆冲断褶皱带、斜歪复式向斜构造和层间滑脱构造带复合控制,砂砾岩型铅锌-铀矿床形成于盆地正反转构造高峰期,而天青石矿床形成于盆地负反转构造期初期。喜山晚期铜-铀成矿亚系统形成于新生代周缘山间咸化湖盆,受前展式薄皮型前陆冲断褶皱带等复合控制。
Multiple deposits of Cu-Pb-Zn-celesite-U-gypsum-coal-gas are enriched in mosaic tectonics of Mesozoic to Cenozoic basin-mountain-plateau,the western Tarim Basin,which is the special intracontinental mineralization element in China.Guided by metallogenic system theoryand theory of wave-mosaic tectonics,based on the method of tectonic lithofacies,the matter-timespace patterns for glutenite-type Cu-Pb-Zn-celesite-U-coal metallogenic system were studied in order to better understand regional metallogenic regularities for this special intracontinental mineralization element.According to the sequences and combinations of tectonic lithofacies,prototype basin and basin dynamics,the glutenite-type Cu-Pb-Zn-celesite-U-coal metallogenic system in the western Tarim Basin may be classified into Yanshanian metallogenic sub-system of Cu-polymetallic-U-coal,Late Yanshanian-Early Himalayan metallogenic sub-system of Pb-Zncelesite-U,and Late Himalayan metallogenic sub-system of Cu-U.Their matter-time-space distributions might be obviously controlled by the compression-extension converting basin in the mosaic tectonics of basin-mountain-plateau,the western Tarim Basin.Yanshanian metallogenic sub-system of Cu-polymetallic-U-coal is located in Cenozoic intracontinent apart-pulled basin,and is synthetically controlled by hedge-type base-involved fold-and-thrust slice,ruched multiple syncline and intrusive tectonic system of gabbro-diabase dykes.They are formed during the stage of basin-positive-inversion,and coupled by positive inversion by thermal materials derived from the upper mantle.Whereas,Late Yanshanian-Early Himalayan metallogenic sub-system of PbZn-celesite-U is located in Cretaceous to Palaeogene compression-extension converting basin,and is synthetically controlled by rear-propagation base-involved fold-and-thrust slice at the southern edge of the southwestern Tianshan,Wulagen inclined synclina and interlayer slip structure.The glutenite-type Pb-Zn-U deposits form during the peak stage of basin-positive-inversion;however,the celesite deposit forms during the beginning stage of basin-negative-inversion.Nevertheless,Late Himalayan metallogenic sub-system of Cu-U is located at Mesozoic intermountain enclosed salted-lake-basin,and is controlled by fold-and-thrust slice belt with piggyback propagation and thin-skin type.
Multiple deposits of Cu-Pb-Zn-celesite-U-gypsum-coal-gas are enriched in mosaic tectonics of Mesozoic to Cenozoic basin-mountain-plateau,the western Tarim Basin,which is the special intracontinental mineralization element in China.Guided by metallogenic system theoryand theory of wave-mosaic tectonics,based on the method of tectonic lithofacies,the matter-timespace patterns for glutenite-type Cu-Pb-Zn-celesite-U-coal metallogenic system were studied in order to better understand regional metallogenic regularities for this special intracontinental mineralization element.According to the sequences and combinations of tectonic lithofacies,prototype basin and basin dynamics,the glutenite-type Cu-Pb-Zn-celesite-U-coal metallogenic system in the western Tarim Basin may be classified into Yanshanian metallogenic sub-system of Cu-polymetallic-U-coal,Late Yanshanian-Early Himalayan metallogenic sub-system of Pb-Zncelesite-U,and Late Himalayan metallogenic sub-system of Cu-U.Their matter-time-space distributions might be obviously controlled by the compression-extension converting basin in the mosaic tectonics of basin-mountain-plateau,the western Tarim Basin.Yanshanian metallogenic sub-system of Cu-polymetallic-U-coal is located in Cenozoic intracontinent apart-pulled basin,and is synthetically controlled by hedge-type base-involved fold-and-thrust slice,ruched multiple syncline and intrusive tectonic system of gabbro-diabase dykes.They are formed during the stage of basin-positive-inversion,and coupled by positive inversion by thermal materials derived from the upper mantle.Whereas,Late Yanshanian-Early Himalayan metallogenic sub-system of PbZn-celesite-U is located in Cretaceous to Palaeogene compression-extension converting basin,and is synthetically controlled by rear-propagation base-involved fold-and-thrust slice at the southern edge of the southwestern Tianshan,Wulagen inclined synclina and interlayer slip structure.The glutenite-type Pb-Zn-U deposits form during the peak stage of basin-positive-inversion;however,the celesite deposit forms during the beginning stage of basin-negative-inversion.Nevertheless,Late Himalayan metallogenic sub-system of Cu-U is located at Mesozoic intermountain enclosed salted-lake-basin,and is controlled by fold-and-thrust slice belt with piggyback propagation and thin-skin type.
引文
[1]刘池洋,毛光周,邱欣卫,等.有机-无机能源矿产相互作用及其共存成藏(矿)[J].自然杂志,2013,35(1):47-55.LIU Chi-yang,MAO Guang-zhou,QIU Xin-wei,et al.Organic-inorganic Energy Minerals Interactions and the Accumulation and Mineralization in the Same Sedimentary Basins[J].Chinese Journal of Nature,2013,35(1):47-55.
[2]刘池洋.沉积盆地动力学与盆地成藏(矿)系统[J].地球科学与环境学报,2008,30(1):1-23.LIU Chi-yang.Dynamics of Sedimentary Basin and Basin Reservoir(Ore)Forming System[J].Journal of Earth Sciences and Environment,2008,30(1):1-23.
[3]薛春纪,高永宝,CHI Guo-xiang,等.滇西北兰坪金顶可能的古油气藏及对铅锌大规模成矿的作用[J].地球科学与环境学报,2009,31(3):221-229.XUE Chun-ji,GAO Yong-bao,CHI Guo-xiang,et al.Possible Former Oil-gas Reservoir in the Giant Jinding Pb-Zn Deposit,Lanping,NW-Yunnan:The Role in the Ore Accumulation[J].Journal of Earth Sciences and Environment,2009,31(3):221-229.
[4]高永宝,薛春纪,曾荣.兰坪金顶铅锌硫化物成矿中硫化氢成因[J].地球科学与环境学报,2008,30(4):367-372.GAO Yong-bao,XUE Chun-ji,ZENG Rong.Forming Mechanism of H2S in the Jinding Pb-Zn Deposit,Lanping Basin,Northwest Yunnan Province[J].Journal of Earth Sciences and Environment,2008,30(4):367-372.
[5]王新利,杨树生,庞艳春,等.云南金顶铅锌矿床成矿物质来源及有机成矿作用[J].地球科学与环境学报,2009,31(4):376-382.WANG Xin-li,YANG Shu-sheng,PANG Yan-chun,et al.Ore Sources and Organic Mineralization in the Jinding Lead-zinc Deposit,Yunnan Province[J].Journal of Earth Sciences and Environment,2009,31(4):376-382.
[6]王丹,吴柏林,寸小妮,等.柴达木盆地多种能源矿产同盆共存及其地质意义[J].地球科学与环境学报,2015,37(3):55-57.WANG Dan,WU Bai-lin,CUN Xiao-ni,et al.Coexistence of Multiple Energy Minerals in Qaidam Basin and Its Geological Significance[J].Journal of Earth Sciences and Environment,2015,37(3):55-57.
[7]贾承造.环青藏高原巨型盆山体系构造与塔里木盆地油气分布规律[J].大地构造与成矿学,2009,33(1):1-9.JIA Cheng-zao.The Structures of Basin and Range System Around the Tibetan Plateau and the Distribution of Oil and Gas in the Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):1-9.
[8]何登发,周新源,杨海军,等.库车坳陷的地质结构及其对大油气田的控制作用[J].大地构造与成矿学,2009,33(1):19-32.HE Deng-fa,ZHOU Xin-yuan,YANG Hai-jun,et al.Geological Structure and Its Controls on Giant Oil and Gas Fields in Kuqa Depression,Tarim Basin:A Clue from New Shot Seismic Data[J].Geotectonica et Metallogenia,2009,33(1):19-32.
[9]何登发,李德生,何金有,等.塔里木盆地库车坳陷和西南坳陷油气地质特征类比及勘探启示[J].石油学报,2013,34(2):202-218.HE Deng-fa,LI De-sheng,HE Jin-you,et al.Comparison in Petroleum Geology Between Kuqa Depression and Southwest Depression in Traim Basin and Its Exploration Significance[J].Acta Petrolei Sinica,2013,34(2):202-218.
[10]刘章月,秦明宽,刘红旭,等.南天山中、新生代造山作用与萨瓦甫齐铀矿床叠加富集效应[J].地质学报,2016,90(12):3310-3323.LIU Zhang-yue,QIN Ming-kuan,LIU Hong-xu,et al.Meso-Cenozoic Orogengy in South Tianshan and the Resultant Superimposed Enrichment Effect on the Sawafuqi Uranium Deposit[J].Acta Geologica Sinica,2016,90(12):3310-3323.
[11]方维萱,贾润幸,郭玉乾,等.塔西地区富烃类还原性盆地流体与砂砾岩型铜铅锌-铀矿床成矿机制[J].地球科学与环境学报,2016,38(6):727-752.FANG Wei-xuan,JIA Run-xing,GUO Yu-qian,et al.Hydrocarbon-rich Basin Fluid with Reductibility and Metallogenic Mechanism for Glutenite-type Cu-PbZn-U Deposits in the Western of Tarim Basin[J].Journal of Earth Sciences and Environment,2016,38(6):727-752.
[12]方维萱,贾润幸,王磊.塔西陆内红层盆地中盆地流体类型、砂砾岩型铜铅锌-铀矿床的大规模褪色化围岩蚀变与金属成矿[J].地球科学与环境学报,2017,39(5):585-619.FANG Wei-xuan,JIA Run-xing,WANG Lei.Types of Basin Fluids,Mechanism of Discolored Alterations and Metal Mineralizations of Glutenite-type Cu-PbZu-U Deposits in Intercontinental Red-bed Basin of the Western Tarim Basin[J].Journal of Earth Sciences and Environment,2017,39(5):585-619.
[13]时文革,巩恩普,褚亦功,等.新疆拜城新近系含铜岩系沉积体系及沉积环境[J].沉积学报,2015,33(6):1074-1086.SHI Wen-ge,GONG En-pu,CHU Yi-gong,et al.Sedimentary System and Depositional Environment of Copper-bearing Rock Series of Neogene in Baicheng County,Xinjiang[J].Acta Sedimentologica Sinica,2015,33(6):1074-1086.
[14]王平户,张国成,解新国.新疆库木库里盆地砂砾岩型铜矿成因分析[J].地质与勘探,2009,45(1):18-22.WANG Ping-hu,ZHANG Guo-cheng,XIE Xin-guo.Genesis of Sandstones-conglomerates Type Copper Deposits at Kumukuli Basin,Xinjiang[J].Geology and Exploration,2009,45(1):18-22.
[15]许桂红,肖昱,田培仁.塔里木盆地周缘中新生代砂岩型铅锌、铜、锰矿区域成矿浅析[J].矿产勘查,2014,5(6):857-865.XU Gui-hong,XIAO Yu,TIAN Pei-ren.Preliminary Discussion of Regional Metallogenic Process of Mesozoic-Cenozoic Sandstone Type Lead-zinc-copper-manganese Deposit in the Tarim Basin,Xinjiang[J].Mineral Exploration,2014,5(6):857-865.
[16]曾威,孙丰月,张雪梅,等.新疆西昆仑特格里曼苏砂岩型铜矿地质特征及成因探讨[J].地质找矿论丛,2012,27(3):284-290.ZENG Wei,SUN Feng-yue,ZHANG Xue-mei,et al.Geological Characteristics of Teglimansu Sandstonehosted Copper Deposit in West Kunlun Mountains in Xinjiang and the Genetic Discussion[J].Contributions to Geology and Mineral Resources Research,2012,27(3):284-290.
[17]黄建国,杨剑,崔春龙,等.塔里木盆地西南缘库斯拉甫一带泥盆纪砂岩型铜矿地质特征:以赛格孜干勒克铜矿为例[J].西北地质,2017,50(2):136-141.HUANG Jian-guo,YANG Jian,CUI Chun-long,et al.Geological Characteristics of Devonian Sandstone-type Copper Deposit in Kusilafu Area,Southwestern Tarim Basin:Evidence from Saifeziganleke Copper Deposit[J].Northwestern Geology,2017,50(2):136-141.
[18]曹养同,杨海军,刘成林,等.库车盆地古-新近纪蒸发岩沉积对喜马拉雅构造运动期次的响应[J].沉积学报,2010,28(6):1054-1065.CAO Yang-tong,YANG Hai-jun,LIU Cheng-lin,et al.Response on Sediment of Evaporate in Kuqa Basin from Paleogene to Neogene Period and Himalayan Tectonic Phase[J].Acta Sedimentologica Sinica,2010,28(6):1054-1065.
[19]张振亮,冯选洁,董福辰,等.西南天山砂砾岩容矿矿床类型及找矿方向[J].西北地质,2014,47(3):70-82.ZHANG Zhen-liang,FENG Xuan-jie,DONG Fu-chen,et al.Genesis and Exploration Direction of Glutenitehosted Ore Deposits in the Southwestern Tianshan Mountains,Xinjiang[J].Northwestern Geology,2014,47(3):70-82.
[20]董连慧,徐兴旺,范廷宾,等.喀喇昆仑火烧云超大型喷流-沉积成因碳酸盐型Pb-Zn矿的发现及区域成矿学意义[J].新疆地质,2015,33(1):41-50.DONG Lian-hui,XU Xing-wang,FAN Ting-bin,et al.Discovery of the Huoshaoyun Super-large Exhalativesedimentary Carbonate Pb-Zn Deposit in the Western Kunlun Area and Its Great Significance for Regional Metallogeny[J].Xinjiang Geology,2015,33(1):41-50.
[21]李文渊.中国西北部成矿地质特征及找矿新发现[J].中国地质,2015,42(3):365-380.LI Wen-yuan.Metallogenic Geological Characteristics and Newly Discovered Orebodies in Northwest China[J].Geology in China,2015,42(3):365-380.
[22]薛春纪,赵晓波,张国震,等.西天山金铜多金属重要成矿类型、成矿环境及找矿潜力[J].中国地质,2015,42(3):381-410.XUE Chun-ji,ZHAO Xiao-bo,ZHANG Guo-zhen,et al.Metallogenic Environments,Ore-forming Types and Prospecting Potential of Au-Cu-Zn-Pb Resources in Western Tianshan Mountains[J].Geology in China,2015,42(3):381-410.
[23]董新丰,薛春纪,李志丹,等.新疆喀什凹陷乌拉根铅锌矿床有机质特征及其地质意义[J].地学前缘,2013,20(1):129-145.DONG Xin-feng,XUE Chun-ji,LI Zhi-dan,et al.Characteristics and Geological Significances of the Organic Matter in the Wulagen Zn-Pb,Kashi Sag,Xinjiang[J].Earth Science Frontiers,2013,20(1):129-145.
[24]韩凤彬,陈正乐,刘增仁,等.西南天山乌拉根铅锌矿床有机地球化学特征及其地质意义[J].矿床地质,2013,32(3):591-602.HAN Feng-bin,CHEN Zheng-le,LIU Zeng-ren,et al.Organic Geochemistry of Wulagen Pb-Zn Deposit in Southwest Tianshan Mountains and Its Implications[J].Mineral Deposits,2013,32(3):591-602.
[25]韩凤彬.新疆乌恰乌拉根铅锌矿床成因研究[D].北京:中国地质科学院,2012.HAN Feng-bin.Study on Metallogensis of Wulagen Lead-zinc Deposit in Wuqia,Xinjiang[D].Beijing:Chinese Academy of Geological Sciences,2012.
[26]韩凤彬,陈正乐,陈柏林,等.新疆喀什凹陷巴什布拉克铀矿流体包裹体及有机地球化学特征[J].中国地质,2012,39(4):985-998.HAN Feng-bin,CHEN Zheng-le,CHEN Bai-lin,et al.Fluid Inclusion and Organic Geochemistry Characteristics of the Bashibulake Uranium Deposit in Kashi Sag,Xinjiang[J].Geology in China,2012,39(4):985-998.
[27]李盛富,陈洪德,蔡根庆,等.巴什布拉克铀矿床物质成分[J].矿物学报,2015,35(3):365-372.LI Sheng-fu,CHEN Hong-de,CAI Gen-qing,et al.Material Composition in Bashibulake Uranium Deposit[J].Acta Mineralogica Sinica,2015,35(3):365-372.
[28]刘章月,秦明宽,蔡根庆,等.新疆巴什布拉克地区有机地球化学特征及其对铀成矿的控制[J].地学前缘,2015,22(4):212-222.LIU Zhang-yue,QIN Ming-kuan,CAI Gen-qing,et al.The Organic Geochemical Characteristics and Its Controls on Uranium Mineralization[J].Earth Science Frontiers,2015,22(4):212-222.
[29]钱俊锋.塔里木盆地西北缘中、新生代构造特征及演化[D].杭州:浙江大学,2008.QIAN Jun-feng.Research on Mesozoic-Cenozoic Structural Characteristics and Evolution in Northwestern Margin,Tarim Basin[D].Hangzhou:Zhejiang University,2008.
[30]陈祖伊,陈戴生,古抗衡,等.中国砂岩型铀矿容矿层位、矿化类型和矿化年龄的区域分布规律[J].铀矿地质,2010,26(6):321-330.CHEN Zu-yi,CHEN Dai-sheng,GU Kang-heng,et al.The Regional Distribution Regularities of Ore-hosting Horizon,Deposit Type and Mineralization Age of China's Sandstone-hosted Uranium Deposits[J].Uranium Geology,2010,26(6):321-330.
[31]刘武生,赵兴齐,史清平,等.中国北方砂岩型铀矿成矿作用与油气关系研究[J].中国地质,2017,44(2):279-287.LIU Wu-sheng,ZHAO Xing-qi,SHI Qing-ping,et al.Research on Relationship of Oil-gas and Sandstonetype Uranium Mineralization of Northern China[J].Geology in China,2017,44(2):279-287.
[32]贾润幸,方维萱,王磊,等.新疆萨热克砂砾岩型铜矿床富烃类还原性盆地流体特征[J].大地构造与成矿学,2017,41(4):1-13.JIA Run-xing,FANG Wei-xuan,WANG Lei,et al.The Characteristics of Reducing Basin Fluid with Rich Hydrocarbon in Sareke Glutenite-type Copper Deposit,Wuqia,Xinjiang[J].Geotectonica et Metallogenia,2017,41(4):1-13.
[33]贾润幸,方维萱,李建旭,等.新疆萨热克铜矿床铼-锇同位素年龄及其地质意义[J].矿床地质,2018,37(1):151-162.JIA Run-xing,FANG Wei-xuan,LI Jian-xu,et al.ReOs Istopic Dating and Its Geological Significance from Sareke Copper Deposit in Wuqia,Xinjiang[J].Mineral Deposit,2018,37(1):151-162.
[34]韩文华,方维萱,张贵山,等.新疆萨热克砂砾岩型铜矿区碎裂岩化相特征[J].地球科学与环境学报,2017,39(3):397-405.HAN Wen-hua,FANG Wei-xuan,ZHANG Gui-shan,et al.Characteristics of Cataclastic Lithofacies in Sareke Glutenite-type Cu Mining Area of Xinjiang,China[J].Journal of Earth Sciences and Environment,2017,39(3):397-405.
[35]王招明,赵孟军,张水昌,等.塔里木盆地西部阿克莫木气田形成初探[J].地质科学,2005,40(2):237-247.WANG Zhao-ming,ZHAO Meng-jun,ZHANG Shuichang,et al.A Preliminary Study on Formation of Akemo Gas Field in the Kashi Sag,Tarim Basin[J].Chinese Journal of Geology,2005,40(2):237-247.
[36]张君峰,王东良,王招明,等.喀什凹陷阿克莫木气田天然气成藏地球化学[J].天然气地球科学,2005,16(4):507-513.ZHANG Jun-feng,WANG Dong-liang,WANG Zhaoming,et al.Natural Gas Deposit Formation Geochemistry of Akmomu Gas Field,Kashi Sag,Tarim Basin[J].Natural Gas Geoscience,2005,16(4):507-513.
[37]达江,宋岩,赵孟军,等.塔里木盆地喀什凹陷北缘烃源岩潜力探讨[J].新疆地质,2007,25(1):77-80.DA Jiang,SONG Yan,ZHAO Meng-jun,et al.Evaluation and Potential Discussion of Hydrocarbon Source Rock in North Margin of Kashi Sag,Tarim Basin[J].Xinjiang Geology,2007,25(1):77-80.
[38]傅国友,宋岩,赵孟军,等.烃源岩对大中型气田形成的控制作用:以塔里木盆地喀什凹陷为例[J].天然气地球科学,2007,18(1):62-66.FU Guo-you,SONG Yan,ZHAO Meng-jun,et al.Analysis of the Controlling Effects of Source Rocks on Middle-large Sized Gas Field Formation:Taking Kashi Sag in Traim Basin as an Example[J].Natural Gas Geoscience,2007,18(1):62-66.
[39]翟裕生.论成矿系统[J].地学前缘,1999,6(1):13-27.ZHAI Yu-sheng.On the Metallogenic System[J].Earth Science Frontiers,1999,6(1):13-27.
[40]翟裕生,王建平,邓军,等.成矿系统时空演化及其找矿意义[J].现代地质,2008,22(2):143-150.ZHAI Yu-sheng,WANG Jian-ping,DENG Jun,et al.Temporal-spatial Evolution of Metallogenic Systems and Its Significance to Mineral Exploration[J].Geoscience,2008,22(2):143-150.
[41]翟裕生.地球系统、成矿系统到勘查系统[J].地学前缘,2007,14(1):172-181.ZHAI Yu-sheng.Earth System,Metallogenic System to Exploration System[J].Earth Science Frontiers,2007,14(1):172-181.
[42]张鸿翔.我国特色成矿系统的研究进展与重点关注的科学问题[J].地球科学进展,2009,24(5):565-570.ZHANG Hong-xiang.The Scientific Progress and Some Key Scientific Problems of Chinese Special Mineralization System[J].Advances in Earth Science,2009,24(5):565-570.
[43]方维萱.对全国生态环境资源进行综合调查评价的设想[J].战略与管理,2018(3/4):20-35.FANG Wei-xuan.Suggestions on Comprehensive Investigations and Assessments on Ecology,Environment,and Resources in China[J].Strategy and Management,2018(3/4):20-35.
[44]方维萱,韩润生.云贵高原-造山带-沉积盆地的构造演化与成岩成矿作用:代序[J].大地构造与成矿学,2014,38(4):729-732.FANG Wei-xuan,HAN Run-sheng.The Geotectonic Evolutions of the Yungui Plateau-orogenic Belt-sedimentary Basin and Its Diagenesis-mineralization:Preface[J].Geotectonica et Metallogenia,2014,38(4):729-732.
[45]张伯声,王战.中国的镶嵌构造与地壳波浪运动[J].西北大学学报:自然科学版,1974,4(1):1-11.ZHANG Bo-sheng,WANG Zhan.Chinese Mosaic Structure and Crust-wave Movement[J].Journal of Northwest University:Natural Science Edition,1974,4(1):1-11.
[46]张伯声,吴文奎.略论塔里木盆地的波浪状镶嵌构造[J].西安地质学院学报,1986,8(3):27-35.ZHANG Bo-sheng,WU Wen-kui.On the Crust-wave Mosaic Structure in the Tarim[J].Journal of Xi'an College of Geology,1986,8(3):27-35.
[47]张伯声,王战.地壳波浪状镶嵌构造学说撮要[J].西安地质学院学报,1993,15(4):6-10.ZHANG Bo-sheng,WANG Zhan.Extraction from Hypothesis of Crust-wave Mosaic Structure[J].Journal of Xi'an College of Geology,1993,15(4):6-10.
[48]方维萱.论热液角砾岩构造系统及研究内容、研究方法和岩相学填图应用[J].大地构造与成矿学,2016,40(2):237-265.FANG Wei-xuan.On Tectonic System of Hydrothermal Breccia:Objective,Methodology and Lithofaciesmapping Applications[J].Geotectonica et Metallogenia,2016,40(2):237-265.
[49]方维萱,王磊,鲁佳,等.新疆萨热克铜矿床绿泥石化蚀变相与构造-岩浆-古地热事件的热通量恢复[J].矿物学报,2017,37(5):661-675.FANG Wei-xuan,WANG Lei,LU Jia,et al.Chloritization Facies and Restoration of Heat Flux for Tectonicmagmatic-thermal Events of Sareke Copper Mine in the Xinjiang Uygur Autonomous Region,China[J].Acta Mineralogica Sinica,2017,37(5):661-675.
[50]方维萱.地球化学岩相学的研究内容、方法与应用实例[J].矿物学报,2017,37(5):509-526.FANG Wei-xuan.Preliminary Research Demonstration on Geochemical Lithofacies:Objective,Methodology,and Case Applications[J].Acta Mineralogica Sinica,2017,37(5):509-526.
[51]罗金海,车自成,张国锋,等.塔里木盆地西北缘与南天山早-中二叠世盆山耦合特征[J].岩石学报,2012,28(8):2506-2514.LUO Jin-hai,CHE Zi-cheng,ZHANG Guo-feng,et al.Early-Middle Permian Basin-mountain Coupling Features Between Northwestern Margin of the Tarim Basin and the South Tianshan Orogeny[J].Acta Petrologica Sinica,2012,28(8):2506-2514.
[52]乔秀夫,李海兵,王思恩,等.新疆境内塔拉斯-费尔干纳断裂早侏罗世走滑的古地震证据[J].地质学报,2008,82(6):721-730.QIAO Xiu-fu,LI Hai-bing,WANG Si-en,et al.Paleoseismic Evidence of the Talas-Ferghana Strike-slip Fault During Early Jurassic,Xinjiang[J].Acta Geologica Sinica,2008,82(6):721-730.
[53]四川省核工业地质调查院.托库依如克幅(K43E024013)1∶50 000区域地质调查报告[R].乌鲁木齐:新疆地质矿产勘查开发局第二地质大队,2010.Sichuan Institute of Nuclear Geology.Tuokuyiruke(K43E024013)Report of Regional Geology Survey at the Scale of 1∶50 000[R].Urumchi:The No.2Geological Team of Xinjiang Bureau of Geological Mineral Exploration and Development,2010.
[54]李永安,李强,张慧,等.塔里木及其周边古地磁研究与盆地形成演化[J].新疆地质,1995,13(4):293-376.LI Yong-an,LI Qiang,ZHANG Hui,et al.Paleomagnetic Study of Tarim and Its Adjacent Area as Well as the Formation and Evolution of Tarim Basin[J].Xinjiang Geology,1995,13(4):293-376.
[55]侯贺晟,高锐,贺日政,等.西南天山-塔里木盆地结合带浅深构造关系:深地震反射剖面的初步揭露[J].地球物理学报,2012,55(12):4116-4125.HOU He-sheng,GAO Rui,HE Ri-zheng,et al.Sallowdeep Tectonic Relationship for the Junction Belt of Western Part of South Tianshan and Tarim Basin:Revealed from Preliminary Processed Deep Seismic Reflection Profile[J].Chinese Journal of Geophyics,2012,55(12):4116-4125.
[56]刘池洋,孙海山.改造型盆地类型划分[J].新疆石油地质,1999,20(2):79-82.LIU Chi-yang,SUN Hai-shan.Classification of Reformed Basin[J].Xinjiang Petroleum Geology,1999,20(2):79-82.
[57]张抗.改造型盆地及其油气地质意义[J].新疆石油地质,1999,20(1):65-70.ZHANG Kang.Reformed Basin and Its Significance in Petroleum Geology[J].Xinjiang Petroleum Geology,1999,20(1):65-70.
[58]MISRA K C.Understanding Mineral Deposit[M].Dordrecht:Kluwer Academic Publishers,1999.
[59]COX D P,LINDSEY D A,SINGER D A,et al.Sedimenthosted Copper Deposits of the World:Deposit Models and Database[R].Reston:USGS,2007.
[60]KIRKHAM R V.Distribution,Settings,and Genesis of Sediment-hosted Stratiform Copper Deposits[C]∥BOYLE R E,BROWN A C,JEFFERSON C W,et al.Sediment-hosted Stratiform Copper Deposits.Toronto:Geological Association of Canada,1989:3-38.
[61]KIRKHAM R V.Volcanic redbed Copper[C]∥ECK-STRAND O R,SINCLAIR W D,THORPE R I.Geology of Canadian Mineral Deposit Types.Ottawa:Geological Survey of Canada,1996:241-252.
[62]张克信,王国灿,曹凯,等.青藏高原新生代主要隆升事件:沉积响应与热年代学记录[J].中国科学:D辑,地球科学,2008,38(12):1575-1588.ZHANG Ke-xin,WANG Guo-can,CAO Kai,et al.Main Uplifting Events of Qingzang:Sedmentary Response and Thermal Chronology Record[J].Science in China:Series D,Earth Sciences,2008,38(12):1575-1588.
[63]SOBEL E R,CHEN J,HEERMANCE R V.Late Oligocene-early Initiation of Shortening in the Southwestern Chinese Tian Shan:Implication for Neogene Shortening Rate Variations[J].Earth and Planetary Science Letters,2006,247(1/2):70-81.
[64]SOBEL E R,DUMITRU T A.Exhumation of the Margins of the Western Tarim Basin During the Himalayan Orogeny[J].Journal of Geophysical Research,1997,102:5043-5064.
[65]FLINT S S.Sediment-hosted Stratabound Copper Deposits of the Central Andes[C]∥BOYLE R E,BROWN A C,JEFFERSON C E,et al.Sedimenthosted Stratiform Copper Deposits.Toronto:Geological Association of Canada,1989:371-398.
[66]刘家铎,王峻,王易斌,等.塔里木盆地喀什北地区白垩系层序岩相古地理特征[J].地球科学与环境学报,2013,35(1):1-14.LIU Jia-duo,WANG Jun,WANG Yi-bin,et al.Sequencelithology Palaeogeography Characteristics of Cretaceous in Northern Kashi Area of Tarim Basin[J].Journal of Earth Sciences and Environment,2013,35(1):1-14.
[67]王二七.关于印度与欧亚大陆初始碰撞时间的讨论[J].中国科学:地球科学,2017,47(3):284-292.WANG Er-qi.A Discussion on the Timing of the Initial Collision Between the Indian and Asian Continents[J].Science China:Earth Sciences,2017,47(3):284-292.
[68]丁林,MAKSATBEK S,蔡福龙,等.印度与欧亚大陆初始碰撞时限、封闭方式和过程[J].中国科学:地球科学,2017,47(3):293-309.DING Lin,MAKSATBEK S,CAI Fu-long,et al.Processes of Initial Collision Andsuturing Between India and Asia[J].Science China:Earth Sciences,2017,47(3):293-309.
[69]李丰收,王伟,杨金明.新疆乌恰县乌拉根铅锌矿床地质地球化学特征及其成因探讨[J].矿产与地质,2005,19(4):335-339.LI Feng-shou,WANG Wei,YANG Jin-ming.Geological and Geochemical Characteristics and Genesis of the Wulagen Lead and Zinc Deposit in Wuqia County,Xinjiang[J].Mineral Resources and Geology,2005,19(4):335-339.
[70]王莹.新疆西南天山地区铅锌矿床区域成矿作用研究[D].北京:中国地质大学,2017.WANG Ying.Mineralization of the Regional Lead-zinc Mineralization in Southwestern Tianshan Area,Xinjiang[D].Beijing:China University of Geosciences,2017.
[71]许志琴,李海兵,杨经绥.造山的高原:青藏高原巨型造山拼贴体和造山类型[J].地学前缘,2006,13(4):1-17.XU Zhi-qin,LI Hai-bing,YANG Jing-sui.An Orogenic Plateau:The Orogenic Collage and Orogenic Types of the Qinghai-Tibet Plateau[J].Earth Science Frontiers,2006,13(4):1-17.
[72]杨克明.论西昆仑大陆边缘构造演化及塔里木西南盆地类型[J].地质论评,1994,40(1):9-18.YANG Ke-ming.The Formation and Evolution of the Western Kunlun Continental Margin[J].Geological Review,1994,40(1):9-18.
[73]陈旭,董玉文,陈红汉,等.塔里木盆地台盆区三叠系三级层序界面和体系域界面的识别与应用[J].沉积学报,2011,29(5):917-927.CHEN Xu,DONG Yu-wen,CHEN Hong-han,et al.Identification and Application of Sequence Boundaries and System Tract Boundaries for the Triassic of Tarim Basin[J].Acta Sedimentologica Sinica,2011,29(5):917-927.
[74]康磊,校培喜,高晓峰,等.西昆仑康西瓦断裂西段斜长片麻岩LA-ICP-MS锆石U-Pb定年及其构造意义[J].地质通报,2012,31(8):1244-1250.KANG Lei,XIAO Pei-xi,GAO Xiao-feng,et al.LA-ICP-MS Zircon U-Pb Dating of Garnet-bearing Muscovite-biotite Plagioclase Gneiss in Western Kangxiwar Fault of Western Kunlun and Its Tectonic Significance[J].Geological Bulletin of China,2012,31(8):1244-1250.
[75]许志琴,戚学祥,杨经绥,等.西昆仑康西瓦韧性走滑剪切带的两类剪切指向、形成时限及其构造意义[J].地质通报,2007,26(10):1252-1261.XU Zhi-qin,QI Xue-xiang,YANG Jing-sui,et al.Senses and Timings of Two Kinds of Shear in the Kangxiwar Strike-slip Shear Zone,West Kunlun,and Their Tectonic Significance[J].Geological Bulletin of China,2007,26(10):1252-1261.
[76]杨文强,刘良,曹玉亭,等.西昆仑塔什库尔干印支期(高压)变质事件的确定及其构造地质意义[J].中国科学:地球科学,2011,41(8):1047-1060.YANG Wen-qiang,LIU Liang,CAO Yu-ting,et al.Geochronological Evidence of Indosinian(High-pressure)Metamorphic Event and Its Tectonic Significance in Taxkorgan Area of the Western Kunlun Mountains,NW China[J].Science China:Earth Sciences,2011,41(8):1047-1060.
[77]张玉泉,朱炳泉,谢应雯,等.青藏高原西部的抬升速率:叶城-狮泉河花岗岩40 Ar-39 Ar年龄的地质解释[J].岩石学报,1998,14(1):11-21.ZHANG Yu-quan,ZHU Bing-quan,XIE Ying-wen,et al.The Uplifting Rates for the Western Qinghai-Xizang Plateau:Interpretation of 40 Ar-39 Ar Dating Data for the Granites in the Area from Yecheng to Shiquanhe[J].Acta Petrologica Sinica,1998,14(1):11-21.
[78]任纪舜.论中国大陆岩石圈构造的基本特征[J].中国区域地质,1991,10(4):289-293.REN Ji-shun.A Discussion on the Basic Features of the Lithosphere Tectonics in Chinese Continent[J].Regional Geology of China,1991,10(4):289-293.
[79]侯增谦,潘桂棠,王安建,等.青藏高原碰撞造山带:Ⅱ.晚碰撞转换成矿作用[J].矿床地质,2006,25(5):521-543.HOU Zeng-qian,PAN Gui-tang,WANG An-jian,et al.Metallogenesis in Tibetan Collisional Orogenic Belt:Ⅱ.Mineralization in Late-collisional Transformation Setting[J].Mineral Deposits,2006,25(5):521-543.
[80]BIRD P.An Updated Digital Model of Plate Boundaries[J].Geochemistry,Geophysics,Geosystems,2003,4(3):1-52.
[81]SHATWELL D.Subducted Ridges,Magmas,Differential Uplift,and Gold Deposits:Examples from South and Central America[R].Canberra:Geoscience Australia,2004.
[82]SISSON V B,PAVLIS T L,ROESKE S M,et al.Introduction:An Overview of Ridge-trench Interactions in Modern and Ancient Settings[C]∥SISSON V B,ROESKE S M,PAVLIS T L.Geology of a Transpressional Orogen Developed During Ridge-trench Interaction Along the North Pacific Margin.Boulder:Geological Society of America,2003:1-18.
[83]ROSENBAUM G,GILES D,SAXON M.Subduction of the Nazca Ridge and the Inca Plateau:Insights into the Formation of Ore Deposits in Peru[J].Earth and Planetary Science Letters,2005,239(1/2):18-32.
[84]MARTINOD J,HUSSON L,ROPERCH P.Horizontal Subduction Zones,Convergence Velocity and the Building of the Andes[J].Earth and Planetary Science Letters,2010,299(3/4):299-309.
[85]GUSTCHER M A,OLIVET J L,ASLANIAN D,et al.The“Lost Inca Plateau”:Cause of Flat Subduction Beneath Peru?[J].Earth and Planetary Science Letters,1999,171(3):335-341.
[86]SILLITE R H,MCKEE E H.Age of Supergene Oxidation and Enrichment in the Chilean Porphyry Copper Province[J].Economic Geology,1996,91:164-179.
[87]MUTSCHLER F E,LUDINGTON S,BOOKSTROMA A.Giant Porphyry-related Metal Camps of the World:A Database[R].Reston:USGS,1999.
[88]韩润生,邹海俊,吴鹏,等.楚雄盆地砂岩型铜矿床构造-流体耦合成矿模型[J].地质学报,2010,84(10):1438-1447.HAN Run-sheng,ZOU Hai-jun,WU Peng,et al.Coupling Tectonic-fluid Metallogenic Model of the Sandstone-type Copper Deposit in the Chuxiong Basin,China[J].Acta Geologica Sinica,2010,84(10):1438-1447.
[89]邹海俊,韩润生,方维萱,等.大姚六苴砂岩型铜矿矿区构造岩矿物岩石学特征与地质意义[J].矿物学报,2017,37(5):528-535.ZOU Hai-jun,HAN Run-sheng,FANG Wei-xuan,et al.Mineralogical-petrological Characteristics of Tectonites from Dayao Liuju Copper Ore-district,Central Yunnan Province,China and Their Geological Significance[J].Acta Mineralogica Sinica,2017,37(5):528-535.
[90]方维萱,王磊,郭玉乾,等.新疆萨热克巴依盆内构造样式及对萨热克大型砂砾岩型铜矿床控制规律[J].地学前缘,2018,25(3):240-259.FANG Wei-xuan,WANG Lei,GUO Yu-qian,et al.Tectonic Patterns in the Sarekebayi Apart-pull Basin and Their Ore-controlling Regularities for the Sareke Glutenite-type Copper Deposit in Xinjiang,China[J].Earth Science Frontiers,2018,25(3):240-259.
[2]刘池洋.沉积盆地动力学与盆地成藏(矿)系统[J].地球科学与环境学报,2008,30(1):1-23.LIU Chi-yang.Dynamics of Sedimentary Basin and Basin Reservoir(Ore)Forming System[J].Journal of Earth Sciences and Environment,2008,30(1):1-23.
[3]薛春纪,高永宝,CHI Guo-xiang,等.滇西北兰坪金顶可能的古油气藏及对铅锌大规模成矿的作用[J].地球科学与环境学报,2009,31(3):221-229.XUE Chun-ji,GAO Yong-bao,CHI Guo-xiang,et al.Possible Former Oil-gas Reservoir in the Giant Jinding Pb-Zn Deposit,Lanping,NW-Yunnan:The Role in the Ore Accumulation[J].Journal of Earth Sciences and Environment,2009,31(3):221-229.
[4]高永宝,薛春纪,曾荣.兰坪金顶铅锌硫化物成矿中硫化氢成因[J].地球科学与环境学报,2008,30(4):367-372.GAO Yong-bao,XUE Chun-ji,ZENG Rong.Forming Mechanism of H2S in the Jinding Pb-Zn Deposit,Lanping Basin,Northwest Yunnan Province[J].Journal of Earth Sciences and Environment,2008,30(4):367-372.
[5]王新利,杨树生,庞艳春,等.云南金顶铅锌矿床成矿物质来源及有机成矿作用[J].地球科学与环境学报,2009,31(4):376-382.WANG Xin-li,YANG Shu-sheng,PANG Yan-chun,et al.Ore Sources and Organic Mineralization in the Jinding Lead-zinc Deposit,Yunnan Province[J].Journal of Earth Sciences and Environment,2009,31(4):376-382.
[6]王丹,吴柏林,寸小妮,等.柴达木盆地多种能源矿产同盆共存及其地质意义[J].地球科学与环境学报,2015,37(3):55-57.WANG Dan,WU Bai-lin,CUN Xiao-ni,et al.Coexistence of Multiple Energy Minerals in Qaidam Basin and Its Geological Significance[J].Journal of Earth Sciences and Environment,2015,37(3):55-57.
[7]贾承造.环青藏高原巨型盆山体系构造与塔里木盆地油气分布规律[J].大地构造与成矿学,2009,33(1):1-9.JIA Cheng-zao.The Structures of Basin and Range System Around the Tibetan Plateau and the Distribution of Oil and Gas in the Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):1-9.
[8]何登发,周新源,杨海军,等.库车坳陷的地质结构及其对大油气田的控制作用[J].大地构造与成矿学,2009,33(1):19-32.HE Deng-fa,ZHOU Xin-yuan,YANG Hai-jun,et al.Geological Structure and Its Controls on Giant Oil and Gas Fields in Kuqa Depression,Tarim Basin:A Clue from New Shot Seismic Data[J].Geotectonica et Metallogenia,2009,33(1):19-32.
[9]何登发,李德生,何金有,等.塔里木盆地库车坳陷和西南坳陷油气地质特征类比及勘探启示[J].石油学报,2013,34(2):202-218.HE Deng-fa,LI De-sheng,HE Jin-you,et al.Comparison in Petroleum Geology Between Kuqa Depression and Southwest Depression in Traim Basin and Its Exploration Significance[J].Acta Petrolei Sinica,2013,34(2):202-218.
[10]刘章月,秦明宽,刘红旭,等.南天山中、新生代造山作用与萨瓦甫齐铀矿床叠加富集效应[J].地质学报,2016,90(12):3310-3323.LIU Zhang-yue,QIN Ming-kuan,LIU Hong-xu,et al.Meso-Cenozoic Orogengy in South Tianshan and the Resultant Superimposed Enrichment Effect on the Sawafuqi Uranium Deposit[J].Acta Geologica Sinica,2016,90(12):3310-3323.
[11]方维萱,贾润幸,郭玉乾,等.塔西地区富烃类还原性盆地流体与砂砾岩型铜铅锌-铀矿床成矿机制[J].地球科学与环境学报,2016,38(6):727-752.FANG Wei-xuan,JIA Run-xing,GUO Yu-qian,et al.Hydrocarbon-rich Basin Fluid with Reductibility and Metallogenic Mechanism for Glutenite-type Cu-PbZn-U Deposits in the Western of Tarim Basin[J].Journal of Earth Sciences and Environment,2016,38(6):727-752.
[12]方维萱,贾润幸,王磊.塔西陆内红层盆地中盆地流体类型、砂砾岩型铜铅锌-铀矿床的大规模褪色化围岩蚀变与金属成矿[J].地球科学与环境学报,2017,39(5):585-619.FANG Wei-xuan,JIA Run-xing,WANG Lei.Types of Basin Fluids,Mechanism of Discolored Alterations and Metal Mineralizations of Glutenite-type Cu-PbZu-U Deposits in Intercontinental Red-bed Basin of the Western Tarim Basin[J].Journal of Earth Sciences and Environment,2017,39(5):585-619.
[13]时文革,巩恩普,褚亦功,等.新疆拜城新近系含铜岩系沉积体系及沉积环境[J].沉积学报,2015,33(6):1074-1086.SHI Wen-ge,GONG En-pu,CHU Yi-gong,et al.Sedimentary System and Depositional Environment of Copper-bearing Rock Series of Neogene in Baicheng County,Xinjiang[J].Acta Sedimentologica Sinica,2015,33(6):1074-1086.
[14]王平户,张国成,解新国.新疆库木库里盆地砂砾岩型铜矿成因分析[J].地质与勘探,2009,45(1):18-22.WANG Ping-hu,ZHANG Guo-cheng,XIE Xin-guo.Genesis of Sandstones-conglomerates Type Copper Deposits at Kumukuli Basin,Xinjiang[J].Geology and Exploration,2009,45(1):18-22.
[15]许桂红,肖昱,田培仁.塔里木盆地周缘中新生代砂岩型铅锌、铜、锰矿区域成矿浅析[J].矿产勘查,2014,5(6):857-865.XU Gui-hong,XIAO Yu,TIAN Pei-ren.Preliminary Discussion of Regional Metallogenic Process of Mesozoic-Cenozoic Sandstone Type Lead-zinc-copper-manganese Deposit in the Tarim Basin,Xinjiang[J].Mineral Exploration,2014,5(6):857-865.
[16]曾威,孙丰月,张雪梅,等.新疆西昆仑特格里曼苏砂岩型铜矿地质特征及成因探讨[J].地质找矿论丛,2012,27(3):284-290.ZENG Wei,SUN Feng-yue,ZHANG Xue-mei,et al.Geological Characteristics of Teglimansu Sandstonehosted Copper Deposit in West Kunlun Mountains in Xinjiang and the Genetic Discussion[J].Contributions to Geology and Mineral Resources Research,2012,27(3):284-290.
[17]黄建国,杨剑,崔春龙,等.塔里木盆地西南缘库斯拉甫一带泥盆纪砂岩型铜矿地质特征:以赛格孜干勒克铜矿为例[J].西北地质,2017,50(2):136-141.HUANG Jian-guo,YANG Jian,CUI Chun-long,et al.Geological Characteristics of Devonian Sandstone-type Copper Deposit in Kusilafu Area,Southwestern Tarim Basin:Evidence from Saifeziganleke Copper Deposit[J].Northwestern Geology,2017,50(2):136-141.
[18]曹养同,杨海军,刘成林,等.库车盆地古-新近纪蒸发岩沉积对喜马拉雅构造运动期次的响应[J].沉积学报,2010,28(6):1054-1065.CAO Yang-tong,YANG Hai-jun,LIU Cheng-lin,et al.Response on Sediment of Evaporate in Kuqa Basin from Paleogene to Neogene Period and Himalayan Tectonic Phase[J].Acta Sedimentologica Sinica,2010,28(6):1054-1065.
[19]张振亮,冯选洁,董福辰,等.西南天山砂砾岩容矿矿床类型及找矿方向[J].西北地质,2014,47(3):70-82.ZHANG Zhen-liang,FENG Xuan-jie,DONG Fu-chen,et al.Genesis and Exploration Direction of Glutenitehosted Ore Deposits in the Southwestern Tianshan Mountains,Xinjiang[J].Northwestern Geology,2014,47(3):70-82.
[20]董连慧,徐兴旺,范廷宾,等.喀喇昆仑火烧云超大型喷流-沉积成因碳酸盐型Pb-Zn矿的发现及区域成矿学意义[J].新疆地质,2015,33(1):41-50.DONG Lian-hui,XU Xing-wang,FAN Ting-bin,et al.Discovery of the Huoshaoyun Super-large Exhalativesedimentary Carbonate Pb-Zn Deposit in the Western Kunlun Area and Its Great Significance for Regional Metallogeny[J].Xinjiang Geology,2015,33(1):41-50.
[21]李文渊.中国西北部成矿地质特征及找矿新发现[J].中国地质,2015,42(3):365-380.LI Wen-yuan.Metallogenic Geological Characteristics and Newly Discovered Orebodies in Northwest China[J].Geology in China,2015,42(3):365-380.
[22]薛春纪,赵晓波,张国震,等.西天山金铜多金属重要成矿类型、成矿环境及找矿潜力[J].中国地质,2015,42(3):381-410.XUE Chun-ji,ZHAO Xiao-bo,ZHANG Guo-zhen,et al.Metallogenic Environments,Ore-forming Types and Prospecting Potential of Au-Cu-Zn-Pb Resources in Western Tianshan Mountains[J].Geology in China,2015,42(3):381-410.
[23]董新丰,薛春纪,李志丹,等.新疆喀什凹陷乌拉根铅锌矿床有机质特征及其地质意义[J].地学前缘,2013,20(1):129-145.DONG Xin-feng,XUE Chun-ji,LI Zhi-dan,et al.Characteristics and Geological Significances of the Organic Matter in the Wulagen Zn-Pb,Kashi Sag,Xinjiang[J].Earth Science Frontiers,2013,20(1):129-145.
[24]韩凤彬,陈正乐,刘增仁,等.西南天山乌拉根铅锌矿床有机地球化学特征及其地质意义[J].矿床地质,2013,32(3):591-602.HAN Feng-bin,CHEN Zheng-le,LIU Zeng-ren,et al.Organic Geochemistry of Wulagen Pb-Zn Deposit in Southwest Tianshan Mountains and Its Implications[J].Mineral Deposits,2013,32(3):591-602.
[25]韩凤彬.新疆乌恰乌拉根铅锌矿床成因研究[D].北京:中国地质科学院,2012.HAN Feng-bin.Study on Metallogensis of Wulagen Lead-zinc Deposit in Wuqia,Xinjiang[D].Beijing:Chinese Academy of Geological Sciences,2012.
[26]韩凤彬,陈正乐,陈柏林,等.新疆喀什凹陷巴什布拉克铀矿流体包裹体及有机地球化学特征[J].中国地质,2012,39(4):985-998.HAN Feng-bin,CHEN Zheng-le,CHEN Bai-lin,et al.Fluid Inclusion and Organic Geochemistry Characteristics of the Bashibulake Uranium Deposit in Kashi Sag,Xinjiang[J].Geology in China,2012,39(4):985-998.
[27]李盛富,陈洪德,蔡根庆,等.巴什布拉克铀矿床物质成分[J].矿物学报,2015,35(3):365-372.LI Sheng-fu,CHEN Hong-de,CAI Gen-qing,et al.Material Composition in Bashibulake Uranium Deposit[J].Acta Mineralogica Sinica,2015,35(3):365-372.
[28]刘章月,秦明宽,蔡根庆,等.新疆巴什布拉克地区有机地球化学特征及其对铀成矿的控制[J].地学前缘,2015,22(4):212-222.LIU Zhang-yue,QIN Ming-kuan,CAI Gen-qing,et al.The Organic Geochemical Characteristics and Its Controls on Uranium Mineralization[J].Earth Science Frontiers,2015,22(4):212-222.
[29]钱俊锋.塔里木盆地西北缘中、新生代构造特征及演化[D].杭州:浙江大学,2008.QIAN Jun-feng.Research on Mesozoic-Cenozoic Structural Characteristics and Evolution in Northwestern Margin,Tarim Basin[D].Hangzhou:Zhejiang University,2008.
[30]陈祖伊,陈戴生,古抗衡,等.中国砂岩型铀矿容矿层位、矿化类型和矿化年龄的区域分布规律[J].铀矿地质,2010,26(6):321-330.CHEN Zu-yi,CHEN Dai-sheng,GU Kang-heng,et al.The Regional Distribution Regularities of Ore-hosting Horizon,Deposit Type and Mineralization Age of China's Sandstone-hosted Uranium Deposits[J].Uranium Geology,2010,26(6):321-330.
[31]刘武生,赵兴齐,史清平,等.中国北方砂岩型铀矿成矿作用与油气关系研究[J].中国地质,2017,44(2):279-287.LIU Wu-sheng,ZHAO Xing-qi,SHI Qing-ping,et al.Research on Relationship of Oil-gas and Sandstonetype Uranium Mineralization of Northern China[J].Geology in China,2017,44(2):279-287.
[32]贾润幸,方维萱,王磊,等.新疆萨热克砂砾岩型铜矿床富烃类还原性盆地流体特征[J].大地构造与成矿学,2017,41(4):1-13.JIA Run-xing,FANG Wei-xuan,WANG Lei,et al.The Characteristics of Reducing Basin Fluid with Rich Hydrocarbon in Sareke Glutenite-type Copper Deposit,Wuqia,Xinjiang[J].Geotectonica et Metallogenia,2017,41(4):1-13.
[33]贾润幸,方维萱,李建旭,等.新疆萨热克铜矿床铼-锇同位素年龄及其地质意义[J].矿床地质,2018,37(1):151-162.JIA Run-xing,FANG Wei-xuan,LI Jian-xu,et al.ReOs Istopic Dating and Its Geological Significance from Sareke Copper Deposit in Wuqia,Xinjiang[J].Mineral Deposit,2018,37(1):151-162.
[34]韩文华,方维萱,张贵山,等.新疆萨热克砂砾岩型铜矿区碎裂岩化相特征[J].地球科学与环境学报,2017,39(3):397-405.HAN Wen-hua,FANG Wei-xuan,ZHANG Gui-shan,et al.Characteristics of Cataclastic Lithofacies in Sareke Glutenite-type Cu Mining Area of Xinjiang,China[J].Journal of Earth Sciences and Environment,2017,39(3):397-405.
[35]王招明,赵孟军,张水昌,等.塔里木盆地西部阿克莫木气田形成初探[J].地质科学,2005,40(2):237-247.WANG Zhao-ming,ZHAO Meng-jun,ZHANG Shuichang,et al.A Preliminary Study on Formation of Akemo Gas Field in the Kashi Sag,Tarim Basin[J].Chinese Journal of Geology,2005,40(2):237-247.
[36]张君峰,王东良,王招明,等.喀什凹陷阿克莫木气田天然气成藏地球化学[J].天然气地球科学,2005,16(4):507-513.ZHANG Jun-feng,WANG Dong-liang,WANG Zhaoming,et al.Natural Gas Deposit Formation Geochemistry of Akmomu Gas Field,Kashi Sag,Tarim Basin[J].Natural Gas Geoscience,2005,16(4):507-513.
[37]达江,宋岩,赵孟军,等.塔里木盆地喀什凹陷北缘烃源岩潜力探讨[J].新疆地质,2007,25(1):77-80.DA Jiang,SONG Yan,ZHAO Meng-jun,et al.Evaluation and Potential Discussion of Hydrocarbon Source Rock in North Margin of Kashi Sag,Tarim Basin[J].Xinjiang Geology,2007,25(1):77-80.
[38]傅国友,宋岩,赵孟军,等.烃源岩对大中型气田形成的控制作用:以塔里木盆地喀什凹陷为例[J].天然气地球科学,2007,18(1):62-66.FU Guo-you,SONG Yan,ZHAO Meng-jun,et al.Analysis of the Controlling Effects of Source Rocks on Middle-large Sized Gas Field Formation:Taking Kashi Sag in Traim Basin as an Example[J].Natural Gas Geoscience,2007,18(1):62-66.
[39]翟裕生.论成矿系统[J].地学前缘,1999,6(1):13-27.ZHAI Yu-sheng.On the Metallogenic System[J].Earth Science Frontiers,1999,6(1):13-27.
[40]翟裕生,王建平,邓军,等.成矿系统时空演化及其找矿意义[J].现代地质,2008,22(2):143-150.ZHAI Yu-sheng,WANG Jian-ping,DENG Jun,et al.Temporal-spatial Evolution of Metallogenic Systems and Its Significance to Mineral Exploration[J].Geoscience,2008,22(2):143-150.
[41]翟裕生.地球系统、成矿系统到勘查系统[J].地学前缘,2007,14(1):172-181.ZHAI Yu-sheng.Earth System,Metallogenic System to Exploration System[J].Earth Science Frontiers,2007,14(1):172-181.
[42]张鸿翔.我国特色成矿系统的研究进展与重点关注的科学问题[J].地球科学进展,2009,24(5):565-570.ZHANG Hong-xiang.The Scientific Progress and Some Key Scientific Problems of Chinese Special Mineralization System[J].Advances in Earth Science,2009,24(5):565-570.
[43]方维萱.对全国生态环境资源进行综合调查评价的设想[J].战略与管理,2018(3/4):20-35.FANG Wei-xuan.Suggestions on Comprehensive Investigations and Assessments on Ecology,Environment,and Resources in China[J].Strategy and Management,2018(3/4):20-35.
[44]方维萱,韩润生.云贵高原-造山带-沉积盆地的构造演化与成岩成矿作用:代序[J].大地构造与成矿学,2014,38(4):729-732.FANG Wei-xuan,HAN Run-sheng.The Geotectonic Evolutions of the Yungui Plateau-orogenic Belt-sedimentary Basin and Its Diagenesis-mineralization:Preface[J].Geotectonica et Metallogenia,2014,38(4):729-732.
[45]张伯声,王战.中国的镶嵌构造与地壳波浪运动[J].西北大学学报:自然科学版,1974,4(1):1-11.ZHANG Bo-sheng,WANG Zhan.Chinese Mosaic Structure and Crust-wave Movement[J].Journal of Northwest University:Natural Science Edition,1974,4(1):1-11.
[46]张伯声,吴文奎.略论塔里木盆地的波浪状镶嵌构造[J].西安地质学院学报,1986,8(3):27-35.ZHANG Bo-sheng,WU Wen-kui.On the Crust-wave Mosaic Structure in the Tarim[J].Journal of Xi'an College of Geology,1986,8(3):27-35.
[47]张伯声,王战.地壳波浪状镶嵌构造学说撮要[J].西安地质学院学报,1993,15(4):6-10.ZHANG Bo-sheng,WANG Zhan.Extraction from Hypothesis of Crust-wave Mosaic Structure[J].Journal of Xi'an College of Geology,1993,15(4):6-10.
[48]方维萱.论热液角砾岩构造系统及研究内容、研究方法和岩相学填图应用[J].大地构造与成矿学,2016,40(2):237-265.FANG Wei-xuan.On Tectonic System of Hydrothermal Breccia:Objective,Methodology and Lithofaciesmapping Applications[J].Geotectonica et Metallogenia,2016,40(2):237-265.
[49]方维萱,王磊,鲁佳,等.新疆萨热克铜矿床绿泥石化蚀变相与构造-岩浆-古地热事件的热通量恢复[J].矿物学报,2017,37(5):661-675.FANG Wei-xuan,WANG Lei,LU Jia,et al.Chloritization Facies and Restoration of Heat Flux for Tectonicmagmatic-thermal Events of Sareke Copper Mine in the Xinjiang Uygur Autonomous Region,China[J].Acta Mineralogica Sinica,2017,37(5):661-675.
[50]方维萱.地球化学岩相学的研究内容、方法与应用实例[J].矿物学报,2017,37(5):509-526.FANG Wei-xuan.Preliminary Research Demonstration on Geochemical Lithofacies:Objective,Methodology,and Case Applications[J].Acta Mineralogica Sinica,2017,37(5):509-526.
[51]罗金海,车自成,张国锋,等.塔里木盆地西北缘与南天山早-中二叠世盆山耦合特征[J].岩石学报,2012,28(8):2506-2514.LUO Jin-hai,CHE Zi-cheng,ZHANG Guo-feng,et al.Early-Middle Permian Basin-mountain Coupling Features Between Northwestern Margin of the Tarim Basin and the South Tianshan Orogeny[J].Acta Petrologica Sinica,2012,28(8):2506-2514.
[52]乔秀夫,李海兵,王思恩,等.新疆境内塔拉斯-费尔干纳断裂早侏罗世走滑的古地震证据[J].地质学报,2008,82(6):721-730.QIAO Xiu-fu,LI Hai-bing,WANG Si-en,et al.Paleoseismic Evidence of the Talas-Ferghana Strike-slip Fault During Early Jurassic,Xinjiang[J].Acta Geologica Sinica,2008,82(6):721-730.
[53]四川省核工业地质调查院.托库依如克幅(K43E024013)1∶50 000区域地质调查报告[R].乌鲁木齐:新疆地质矿产勘查开发局第二地质大队,2010.Sichuan Institute of Nuclear Geology.Tuokuyiruke(K43E024013)Report of Regional Geology Survey at the Scale of 1∶50 000[R].Urumchi:The No.2Geological Team of Xinjiang Bureau of Geological Mineral Exploration and Development,2010.
[54]李永安,李强,张慧,等.塔里木及其周边古地磁研究与盆地形成演化[J].新疆地质,1995,13(4):293-376.LI Yong-an,LI Qiang,ZHANG Hui,et al.Paleomagnetic Study of Tarim and Its Adjacent Area as Well as the Formation and Evolution of Tarim Basin[J].Xinjiang Geology,1995,13(4):293-376.
[55]侯贺晟,高锐,贺日政,等.西南天山-塔里木盆地结合带浅深构造关系:深地震反射剖面的初步揭露[J].地球物理学报,2012,55(12):4116-4125.HOU He-sheng,GAO Rui,HE Ri-zheng,et al.Sallowdeep Tectonic Relationship for the Junction Belt of Western Part of South Tianshan and Tarim Basin:Revealed from Preliminary Processed Deep Seismic Reflection Profile[J].Chinese Journal of Geophyics,2012,55(12):4116-4125.
[56]刘池洋,孙海山.改造型盆地类型划分[J].新疆石油地质,1999,20(2):79-82.LIU Chi-yang,SUN Hai-shan.Classification of Reformed Basin[J].Xinjiang Petroleum Geology,1999,20(2):79-82.
[57]张抗.改造型盆地及其油气地质意义[J].新疆石油地质,1999,20(1):65-70.ZHANG Kang.Reformed Basin and Its Significance in Petroleum Geology[J].Xinjiang Petroleum Geology,1999,20(1):65-70.
[58]MISRA K C.Understanding Mineral Deposit[M].Dordrecht:Kluwer Academic Publishers,1999.
[59]COX D P,LINDSEY D A,SINGER D A,et al.Sedimenthosted Copper Deposits of the World:Deposit Models and Database[R].Reston:USGS,2007.
[60]KIRKHAM R V.Distribution,Settings,and Genesis of Sediment-hosted Stratiform Copper Deposits[C]∥BOYLE R E,BROWN A C,JEFFERSON C W,et al.Sediment-hosted Stratiform Copper Deposits.Toronto:Geological Association of Canada,1989:3-38.
[61]KIRKHAM R V.Volcanic redbed Copper[C]∥ECK-STRAND O R,SINCLAIR W D,THORPE R I.Geology of Canadian Mineral Deposit Types.Ottawa:Geological Survey of Canada,1996:241-252.
[62]张克信,王国灿,曹凯,等.青藏高原新生代主要隆升事件:沉积响应与热年代学记录[J].中国科学:D辑,地球科学,2008,38(12):1575-1588.ZHANG Ke-xin,WANG Guo-can,CAO Kai,et al.Main Uplifting Events of Qingzang:Sedmentary Response and Thermal Chronology Record[J].Science in China:Series D,Earth Sciences,2008,38(12):1575-1588.
[63]SOBEL E R,CHEN J,HEERMANCE R V.Late Oligocene-early Initiation of Shortening in the Southwestern Chinese Tian Shan:Implication for Neogene Shortening Rate Variations[J].Earth and Planetary Science Letters,2006,247(1/2):70-81.
[64]SOBEL E R,DUMITRU T A.Exhumation of the Margins of the Western Tarim Basin During the Himalayan Orogeny[J].Journal of Geophysical Research,1997,102:5043-5064.
[65]FLINT S S.Sediment-hosted Stratabound Copper Deposits of the Central Andes[C]∥BOYLE R E,BROWN A C,JEFFERSON C E,et al.Sedimenthosted Stratiform Copper Deposits.Toronto:Geological Association of Canada,1989:371-398.
[66]刘家铎,王峻,王易斌,等.塔里木盆地喀什北地区白垩系层序岩相古地理特征[J].地球科学与环境学报,2013,35(1):1-14.LIU Jia-duo,WANG Jun,WANG Yi-bin,et al.Sequencelithology Palaeogeography Characteristics of Cretaceous in Northern Kashi Area of Tarim Basin[J].Journal of Earth Sciences and Environment,2013,35(1):1-14.
[67]王二七.关于印度与欧亚大陆初始碰撞时间的讨论[J].中国科学:地球科学,2017,47(3):284-292.WANG Er-qi.A Discussion on the Timing of the Initial Collision Between the Indian and Asian Continents[J].Science China:Earth Sciences,2017,47(3):284-292.
[68]丁林,MAKSATBEK S,蔡福龙,等.印度与欧亚大陆初始碰撞时限、封闭方式和过程[J].中国科学:地球科学,2017,47(3):293-309.DING Lin,MAKSATBEK S,CAI Fu-long,et al.Processes of Initial Collision Andsuturing Between India and Asia[J].Science China:Earth Sciences,2017,47(3):293-309.
[69]李丰收,王伟,杨金明.新疆乌恰县乌拉根铅锌矿床地质地球化学特征及其成因探讨[J].矿产与地质,2005,19(4):335-339.LI Feng-shou,WANG Wei,YANG Jin-ming.Geological and Geochemical Characteristics and Genesis of the Wulagen Lead and Zinc Deposit in Wuqia County,Xinjiang[J].Mineral Resources and Geology,2005,19(4):335-339.
[70]王莹.新疆西南天山地区铅锌矿床区域成矿作用研究[D].北京:中国地质大学,2017.WANG Ying.Mineralization of the Regional Lead-zinc Mineralization in Southwestern Tianshan Area,Xinjiang[D].Beijing:China University of Geosciences,2017.
[71]许志琴,李海兵,杨经绥.造山的高原:青藏高原巨型造山拼贴体和造山类型[J].地学前缘,2006,13(4):1-17.XU Zhi-qin,LI Hai-bing,YANG Jing-sui.An Orogenic Plateau:The Orogenic Collage and Orogenic Types of the Qinghai-Tibet Plateau[J].Earth Science Frontiers,2006,13(4):1-17.
[72]杨克明.论西昆仑大陆边缘构造演化及塔里木西南盆地类型[J].地质论评,1994,40(1):9-18.YANG Ke-ming.The Formation and Evolution of the Western Kunlun Continental Margin[J].Geological Review,1994,40(1):9-18.
[73]陈旭,董玉文,陈红汉,等.塔里木盆地台盆区三叠系三级层序界面和体系域界面的识别与应用[J].沉积学报,2011,29(5):917-927.CHEN Xu,DONG Yu-wen,CHEN Hong-han,et al.Identification and Application of Sequence Boundaries and System Tract Boundaries for the Triassic of Tarim Basin[J].Acta Sedimentologica Sinica,2011,29(5):917-927.
[74]康磊,校培喜,高晓峰,等.西昆仑康西瓦断裂西段斜长片麻岩LA-ICP-MS锆石U-Pb定年及其构造意义[J].地质通报,2012,31(8):1244-1250.KANG Lei,XIAO Pei-xi,GAO Xiao-feng,et al.LA-ICP-MS Zircon U-Pb Dating of Garnet-bearing Muscovite-biotite Plagioclase Gneiss in Western Kangxiwar Fault of Western Kunlun and Its Tectonic Significance[J].Geological Bulletin of China,2012,31(8):1244-1250.
[75]许志琴,戚学祥,杨经绥,等.西昆仑康西瓦韧性走滑剪切带的两类剪切指向、形成时限及其构造意义[J].地质通报,2007,26(10):1252-1261.XU Zhi-qin,QI Xue-xiang,YANG Jing-sui,et al.Senses and Timings of Two Kinds of Shear in the Kangxiwar Strike-slip Shear Zone,West Kunlun,and Their Tectonic Significance[J].Geological Bulletin of China,2007,26(10):1252-1261.
[76]杨文强,刘良,曹玉亭,等.西昆仑塔什库尔干印支期(高压)变质事件的确定及其构造地质意义[J].中国科学:地球科学,2011,41(8):1047-1060.YANG Wen-qiang,LIU Liang,CAO Yu-ting,et al.Geochronological Evidence of Indosinian(High-pressure)Metamorphic Event and Its Tectonic Significance in Taxkorgan Area of the Western Kunlun Mountains,NW China[J].Science China:Earth Sciences,2011,41(8):1047-1060.
[77]张玉泉,朱炳泉,谢应雯,等.青藏高原西部的抬升速率:叶城-狮泉河花岗岩40 Ar-39 Ar年龄的地质解释[J].岩石学报,1998,14(1):11-21.ZHANG Yu-quan,ZHU Bing-quan,XIE Ying-wen,et al.The Uplifting Rates for the Western Qinghai-Xizang Plateau:Interpretation of 40 Ar-39 Ar Dating Data for the Granites in the Area from Yecheng to Shiquanhe[J].Acta Petrologica Sinica,1998,14(1):11-21.
[78]任纪舜.论中国大陆岩石圈构造的基本特征[J].中国区域地质,1991,10(4):289-293.REN Ji-shun.A Discussion on the Basic Features of the Lithosphere Tectonics in Chinese Continent[J].Regional Geology of China,1991,10(4):289-293.
[79]侯增谦,潘桂棠,王安建,等.青藏高原碰撞造山带:Ⅱ.晚碰撞转换成矿作用[J].矿床地质,2006,25(5):521-543.HOU Zeng-qian,PAN Gui-tang,WANG An-jian,et al.Metallogenesis in Tibetan Collisional Orogenic Belt:Ⅱ.Mineralization in Late-collisional Transformation Setting[J].Mineral Deposits,2006,25(5):521-543.
[80]BIRD P.An Updated Digital Model of Plate Boundaries[J].Geochemistry,Geophysics,Geosystems,2003,4(3):1-52.
[81]SHATWELL D.Subducted Ridges,Magmas,Differential Uplift,and Gold Deposits:Examples from South and Central America[R].Canberra:Geoscience Australia,2004.
[82]SISSON V B,PAVLIS T L,ROESKE S M,et al.Introduction:An Overview of Ridge-trench Interactions in Modern and Ancient Settings[C]∥SISSON V B,ROESKE S M,PAVLIS T L.Geology of a Transpressional Orogen Developed During Ridge-trench Interaction Along the North Pacific Margin.Boulder:Geological Society of America,2003:1-18.
[83]ROSENBAUM G,GILES D,SAXON M.Subduction of the Nazca Ridge and the Inca Plateau:Insights into the Formation of Ore Deposits in Peru[J].Earth and Planetary Science Letters,2005,239(1/2):18-32.
[84]MARTINOD J,HUSSON L,ROPERCH P.Horizontal Subduction Zones,Convergence Velocity and the Building of the Andes[J].Earth and Planetary Science Letters,2010,299(3/4):299-309.
[85]GUSTCHER M A,OLIVET J L,ASLANIAN D,et al.The“Lost Inca Plateau”:Cause of Flat Subduction Beneath Peru?[J].Earth and Planetary Science Letters,1999,171(3):335-341.
[86]SILLITE R H,MCKEE E H.Age of Supergene Oxidation and Enrichment in the Chilean Porphyry Copper Province[J].Economic Geology,1996,91:164-179.
[87]MUTSCHLER F E,LUDINGTON S,BOOKSTROMA A.Giant Porphyry-related Metal Camps of the World:A Database[R].Reston:USGS,1999.
[88]韩润生,邹海俊,吴鹏,等.楚雄盆地砂岩型铜矿床构造-流体耦合成矿模型[J].地质学报,2010,84(10):1438-1447.HAN Run-sheng,ZOU Hai-jun,WU Peng,et al.Coupling Tectonic-fluid Metallogenic Model of the Sandstone-type Copper Deposit in the Chuxiong Basin,China[J].Acta Geologica Sinica,2010,84(10):1438-1447.
[89]邹海俊,韩润生,方维萱,等.大姚六苴砂岩型铜矿矿区构造岩矿物岩石学特征与地质意义[J].矿物学报,2017,37(5):528-535.ZOU Hai-jun,HAN Run-sheng,FANG Wei-xuan,et al.Mineralogical-petrological Characteristics of Tectonites from Dayao Liuju Copper Ore-district,Central Yunnan Province,China and Their Geological Significance[J].Acta Mineralogica Sinica,2017,37(5):528-535.
[90]方维萱,王磊,郭玉乾,等.新疆萨热克巴依盆内构造样式及对萨热克大型砂砾岩型铜矿床控制规律[J].地学前缘,2018,25(3):240-259.FANG Wei-xuan,WANG Lei,GUO Yu-qian,et al.Tectonic Patterns in the Sarekebayi Apart-pull Basin and Their Ore-controlling Regularities for the Sareke Glutenite-type Copper Deposit in Xinjiang,China[J].Earth Science Frontiers,2018,25(3):240-259.