中亚南天山穆龙套型金矿地质背景、成矿特征和找矿策略
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摘要
中亚南天山是世界上最重要的金矿带,以浅变质含碳质碎屑岩系为容矿岩石的穆龙套型金矿最为发育且规模巨大。将境内外南天山作为整体开展研究,有助于推进中国新疆南天山地区金矿的找矿持续突破。南天山是南天山洋在石炭纪末闭合时在Karakum—塔里木板块北缘形成的褶皱冲断带。南天山地区穆龙套型金矿的容矿地层为一套浅变质、变形强烈的含碳质细碎屑岩建造,对金矿化有明显预富集;区域内的大型韧-脆性变形带,剪切带及相关断裂系统是穆龙套型金矿的控矿构造;金矿区岩浆活动虽然较弱,但岩浆活动与成矿具有紧密的时空联系。矿体呈脉状、板状、透镜状,常以黄铁矿和毒砂为主要载金矿物,围岩蚀变以硅化、黄铁矿化、碳酸盐化最为发育。成矿年龄多为晚古生代,同位素示踪指示成矿流体、硫及成矿金属物质具有壳幔混源特征。"碳质岩系+构造变形+岩浆热液"是穆龙套型金成矿的关键控制因素。按照总体控矿特征,探讨了中国新疆南天山地区穆龙套型金矿床的主要找矿策略。
The Southern Tianshan area in Central Asia is the most important gold metallogenic belt in the word and the shallow metamorphic carbonaceous metamorphic rock-hosted Muruntau-type gold deposits are widely developed here.Generally such type of gold deposit is gigantic.Taking the whole Southern Tianshan as the study area,both areas inside and outside the border of China will help to make breakthrough of gold prospecting in the Southern Tianshan area of Xinjiang.The whole Southern Tianshan area was a fold thrust belt at the North margin of Karakum-Tarim Plate formed during the Southern Tianshan ocean closure in Late Carboniferous Period.Gold is pre-enriched in the host rock(the shallow metamorphic but strongly deformed carbonaceous metamorphic fine-grained clastic rock)of Muruntau-type gold deposit.Such type gold deposit in the area is controlled by large ductile-brittle deformation zone,shear zone and related fault system.Mineralization is closely related in time and space although magmatism in the mining area looks weak.Ore body is generally vein like,tabular and lenticular.Pyrite and aesenopyrite are the main gold-carriers.The mostly developed wallrock alteration is silicification,pyritization and carbonation.Most age data fall in Late Palaeozoic Era.Isotope tracing is characterized by crut-mantle mixture source of ore fluid,sulfur and ore metals.Prospecting strateg is discussed on basis of the comprehensive control factor,i.e.Carbonaceous rock+structure deformation+magmatism.
The Southern Tianshan area in Central Asia is the most important gold metallogenic belt in the word and the shallow metamorphic carbonaceous metamorphic rock-hosted Muruntau-type gold deposits are widely developed here.Generally such type of gold deposit is gigantic.Taking the whole Southern Tianshan as the study area,both areas inside and outside the border of China will help to make breakthrough of gold prospecting in the Southern Tianshan area of Xinjiang.The whole Southern Tianshan area was a fold thrust belt at the North margin of Karakum-Tarim Plate formed during the Southern Tianshan ocean closure in Late Carboniferous Period.Gold is pre-enriched in the host rock(the shallow metamorphic but strongly deformed carbonaceous metamorphic fine-grained clastic rock)of Muruntau-type gold deposit.Such type gold deposit in the area is controlled by large ductile-brittle deformation zone,shear zone and related fault system.Mineralization is closely related in time and space although magmatism in the mining area looks weak.Ore body is generally vein like,tabular and lenticular.Pyrite and aesenopyrite are the main gold-carriers.The mostly developed wallrock alteration is silicification,pyritization and carbonation.Most age data fall in Late Palaeozoic Era.Isotope tracing is characterized by crut-mantle mixture source of ore fluid,sulfur and ore metals.Prospecting strateg is discussed on basis of the comprehensive control factor,i.e.Carbonaceous rock+structure deformation+magmatism.
引文
[1]涂光炽.初议中亚成矿域[J].地质科学,1999(4):397-404.
[2]Porter T M.An overview of the world's porphyry of other hydrothermal Cu and Au deposits and their distribution[J].Porphyry and hydrothermal Cu Au deposits-A global perspective,Conference Proceedings,1998:3-17.
[3]薛春纪,赵晓波,莫宣学,等.西天山“亚洲金腰带”及其动力背景和成矿控制与找矿[J].地学前缘,2014,21(5):128-155.
[4]刘德权,唐延龄,周汝洪.新疆穆龙套型金矿的找矿方向[J].黄金科学技术,1998,6(1):18-23.
[5]戴自希,白冶,吴初国,等.中国西部和毗邻国家铜金找矿潜力的对比研究[M].北京:地震出版社,2001:57-73.
[6]陈哲夫.新疆与邻区南天山超大型金矿成矿条件和找矿方向[J].新疆地质,2002,20(3):229-232.
[7]刘家军,郑明华,龙训荣,等.新疆萨瓦亚尔顿穆龙套型金矿床的确认及其意义[J].贵金属地质,2000,9(3):129-143.
[8]鲍庆中,沙德铭,王宏.也谈南天山古生代造山带内穆龙套型金矿床的控矿因素和找矿方向[J].地质与资源,2003,12(3):159-165.
[9]杨富全,王义天,李蒙文,等.新疆天山黑色岩系型矿床的地质特征及找矿方向[J].地质通报,2005,24(5):462-469.
[10]刘春涌,王永江.初论中亚黑色岩系型金矿床的基本特征——兼论新疆黑色岩系型金矿找矿方向[J].新疆地质,2007,25(1):34-39.
[11]Groves D I,Goldfarb R J,Gebre-Mariam M,et al.Orogenic gold deposits:A proposed classification in the context of their crustal distribution and relationship to other gold deposit types[J].Ore Geology Reviews,1998,13(1):7-27.
[12]Goldfarb R J,Groves D I,Gardoll S.Orogenic gold and geologic time:aglobal synthesis[J].Ore Geology Reviews,2001,18(1):1-75.
[13]Kempe U,Belyatsky B V,Krymsky R S,et al.Sm-Nd and Sr isotope systematics of scheelite from the giant Au(-W)deposit Muruntau(Uzbekistan):implications for the age and sources of Au mineralization[J].Mineralium Deposita,2001,36(5):379-392.
[14]Bierlein F P,Groves D I,Goldfarb R J,et al.Lithospheric controls on the formation of provinces hosting giant orogenic gold deposits[J].Mineralium Deposita,2006,40(8):874-886.
[15]Frimmel H E.Earth's continental crustal gold endowment[J].Earth and Planetary Science Letters,2008,267(1):45-55.
[16]陈华勇,陈衍景,倪培,等.南天山萨瓦亚尔顿金矿流体包裹体研究:矿床成因和勘探意义[J].矿物岩石,2004,24(3):46-54.
[17]陈华勇,陈衍景,倪培,等.新疆萨瓦亚尔顿金矿流体包裹体成分、矿床成因和成矿预测[J].岩石学报,2007,23(9):2189-2197.
[18]薛春纪,赵晓波,莫宣学,等.西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J].地质学报,2014,88(12):2490-2531.
[19]毛景文,韩春明,王义天,等.中亚地区南天山大型金矿带的地质特征、成矿模型和勘查准则[J].地质通报,2002,21(1):858-867.
[20]Mao J,Konopelko D,Seltmann R,et al.Post collisional Age of the Kumtor Gold Deposit and Timing of Hercynian Events in the Tien Shan,Kyrgyzstan[J].Economic Geology,2004,99:1771-1780.
[21]Pasava J,Frimmel H,VymazalováA,et al.A two-stage evolution model for the Amantaytau orogenic-type gold deposit in Uzbekistan[J].Mineralium Deposita,2013,48:825-840.
[22]Liu J,Zheng M,Cook N J,et al.Geological and geochemical characteristics of the Sawaya'erdun gold deposit,southwestern Chinese Tianshan[J].Ore Geology Reviews,2007,32(1):125-156.
[23]杨富全.西南天山金矿成矿条件及成矿机制[D].北京:中国地质科学院,2005:1-186.
[24]Drew L J,Berger B R,Kurbanov N K.Geology and structural evolution of the Muruntau gold deposit,Kyzylkum desert,Uzbekistan[J].Ore Geology Reviews,1996,11(4):175-196.
[25]Graupner T,Kempe U,Spooner E T C,et al.Microthermometric,Laser Raman Spectroscopic,and Volatile-Ion Chromatographic Analysis of Hydrothermal Fluids in the Paleozoic Muruntau Au-Bearing Quartz Vein Ore Field,Uzbekistan[J].Economic Geology,2001,96:1-23.
[26]Wilde A R,Layer P,Mernagh T,et al.The Giant Muruntau Gold Deposit:Geologic,Geochronologic,and Fluid Inclusion Constraints on Ore Genesis[J].Economic Geology,2001,96(3):633-644.
[27]Graupner T,Niedermann S,Kempe U,et al.Origin of ore fluids in the Muruntau gold system:Constraints from noble gas,carbon isotope and halogen data[J].Geochimica et Cosmochimica Acta,2006,70(21):5356-5370.
[28]Morelli R,Creaser R A,Seltmann R,et al.Age and source constraints for the giant Muruntau gold deposit,Uzbekistan,from coupled Re-Os-He isotopes in arsenopyrite[J].Geology,2007,35(9):795-798.
[29]Yang F,Mao J,Wang Y,et al.Geology and Metallogenesis of the Sawayaerdun Gold Deposit in the Southwestern Tianshan Mountains,Xinjiang,China[J].Resource Geology,2007,57(1):57-75.
[30]叶锦华,王立本,叶庆同,等.西南天山萨瓦亚尔顿金(锑)矿床成矿时代与赋矿地层时代[J].地球学报,1999,20(3):278-283.
[31]叶锦华,叶庆同,王进,等.萨瓦亚尔顿金(锑)矿床地质地球化学特征与成矿机理探讨[J].矿床地质,1999,18(1):63-72.
[32]郑明华,刘家军,张寿庭,等.萨瓦亚尔顿金矿床的同位素组成特征及其成因意义[J].成都理工学院学报,2002,11(3):140-146.
[33]杨富全,毛景文,王义天,等.新疆萨瓦亚尔顿金矿床年代学、氦氩碳氧同位素特征及其地质意义[J].地质论评,2006,52(3):341-351.
[34]Chen H Y,Chen Y J,Baker M.Isotopic geochemistry of the Sawayaerdun orogenic-type gold deposit,Tianshan,northwest China:Implications for ore genesis and mineral exploration[J].Chemical Geology,2012,310/311:1-11.
[35]杨富全,叶庆同,傅旭杰,等.新疆西南天山金矿分布、类型和成矿条件[J].新疆地质,1999,17(2):129-136.
[36]杨富全,毛景文,王义天,等.新疆西南天山金矿床主要类型、特征及成矿作用[J].矿床地质,2007,26(4):361-379.
[37]杨在峰,朱志新,王克卓,等.新疆西天山地区黑色岩系金矿成矿地质特征及找矿潜力分析[J].新疆地质,2008,26(3):247-252.
[38]聂凤军,江思宏,侯万荣,等.内蒙古中西部浅变质岩为容矿围岩的金矿床地质特征及形成过程[J].矿床地质,2010,29(1):58-70.
[39]高俊,龙灵利,钱青,等.南天山:晚古生代还是三叠纪碰撞造山带[J].岩石学报,2006,22(5):1049-1061.
[40]Sengor A M C,Natal'in B A.Turkic-type orogeny and its role in the making of the continental crust[J].Annual Reviews of Earth and Planetary Sciences,1996,24:263-337.
[41]Xiao W J,Han C M,Yuan C,et al.Middle Cambrian to Permian subduction-related accretionary orogenesis of Northern Xinjiang,NW China:Implications for the tectonic evolution of central Asia[J].Journal of Asian Earth Science,2008,32:102-117.
[42]Xiao W J,Kr9ner A,Windley B F.Geodynamic evolution of Central Asia in the Paleozoic and Mesozoic[J].International Journal of Earth Sciences,2009,98:1185-1188.
[43]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.
[44]王超,刘良,车自成,等.西南天山阔克萨彦岭巴雷公镁铁质岩石的地球化学特征:LA-ICP-MS U-Pb年龄及其大地构造意义[J].地质论评,2007,53(6):743-754.
[45]Wang B,Shu L S,Faure M,et al.Paleozoic tectonics of the southern Chinese Tianshan:insights from structural,chronological and geochemical studies of the Heiyingshan ophiolitic mélange(NW China)[J].Tectonophysics,2011,497:85-104.
[46]Han B F,He G Q,Wang X C,et al.Late Carboniferous collision between the Tarim and Kazakhstan-Yili terranes in the western segment of the South TianShan Orogen,Central Asia,and implications for the Northern Xinjiang,western China[J].Earth-Science Reviews,2011,109:74-93.
[47]龙灵利,高俊,熊贤明,等.南天山库勒湖蛇绿岩地球化学特征及其年龄[J].岩石学报,2006,22(1):65-73.
[48]马中平,夏林圻,徐学义,等.南天山库勒湖蛇绿岩锆石年龄及其地质意义[J].西北大学学报(自然科学版),2007,37(1):107-110.
[49]张成立,周鼎武,王居里,等.南天山库米什南黄尖石山岩体的年代学、地球化学和Sr、Nd同位素组成及其成因意义[J].岩石学报,2007,23(8):1821-1829.
[50]Mirkamalov R K,Isokov M U,Chirikin V V,et al.New results of U-Pb(SHRIMP)dating of Granitoid and Methamophic complexs of the Tien Shan Folded Belt[C]∥Kbarov Kh A A,Nurtaev B S.Geosciences in Uzbekistan,Tashkent,2012:114-125.
[51]Gao J,Klemd R.Formation of HP-LT rocks and their tectonic implications in the western Tianshan Orogen,NW China:geochemical and age constraints[J].Lithos,2003,66:1-22.
[52]Hegner E,Klemd R,Kr9ner A,et al.Mineralogy ages and P-T conditions of late Paleozoic high-pressure eclogite and provenance of mélange sediments in the South Tianshan Orogen of Kyrgyzstan[J].American Journal of Science,2010,310:916-950.
[53]Su W,Gao J,Klemd R,et al.U-Pb zircon geochronology of Tianshan eclogites in NW China:implication for the collision between the Yili and Tarim blocks of the southwestern Altaids[J].European Journal of Mineralogy,2010,22:473-478.
[54]Li Q L,Lin W,Su W,et al.SIMS U-Pb rutile age of lowtemperature eclogites from southwestern Chinese Tianshan,NW China[J].Lithos,2011,122:76-86.
[55]Klemd R,Br9cker M,Hacker B R,et al.New age constraints on the metamorphic evolution of the high-pressure/low-temperature belt in the western Tianshan Mountains,NWChina[J].Journal of Geology,2005,113:157-168.
[56]Zverev Yu,Kremenetsky A,Minzer E,et al.The Amantaytau—Daughyztau ore field[C]∥Shayakubov T,Islamov F,Kremenetsky A,et al.Au,Ag and Cu deposits of Uzbekistan.Excursion Guidebook,International Field Conference of IGCP-373,Excursion B6of the Joint SGA-IAGOD Symposium,London/Tashkent,1999,27/28,August-4September:17-74.
[57]Wall V J,Yantzen V,Graupner T,et al.Muruntau,Uzbekistan Report on CERCAMS Research Project[R].2004:1-96.
[58]Kostitsyn Y A.Rb-Sr isotopic study of the Muruntau deposit:Magmatism,metamorphism,and mineralization[J]:Geochemistry International,1996,34:1009-1023.
[59]Bagdasaryan A G,Fedyanin A S,Shemetov P A.Estimate of the formation time and other parameters of a disruption structure in open pit walls in terms of Muruntau open pit[J].Journal of Mining Science,2009,45(2):146-151.
[60]谭娟娟,朱永峰.穆龙套金矿地质和地球化学[J].矿物岩石地球化学通报,2008,27(4):391-398.
[61]孟广路,王斌,李宝强,等.乌兹别克斯坦穆龙套金矿床研究进展[J].地质科技情报,2013,32(5):160-166.
[62]Zverev Yu,Kremenetsky A,Minzer E,et al.The Amantaytau—Daughyztau ore field[C]∥Shayakubov T,Islamov F,Kremenetsky A,Seltmann R(eds).Au,Ag,and Cu deposits of Uzbekistan.Excursion guidebook,International Field Conference of IGCP-373,Excursion B6of the Joint SGA-IAGOD Symposium,London/Tashkent,1999,27/28,August–4September:17-35.
[63]Kurbanov N K,Romanov V L,Arifulov C R R,et al.Geological guidebook to the gold deposits of Uzbekistan(for the USGS)[M].Central Research Institute of Geological Prospecting for Base and Precious Meas(TsNIGRI),Moscow,1991:19.
[64]Nikonorov V V,Karaev Y V,Borisov F I,et al.Gold resources of Kyrgyzstan[M].Bishkek,2007:1-500.
[65]Ansdell K M,Abeleira A,Ivanov S.Structural evolution and vein paragenesis at the Kumtor gold deposit,Kyrgyzstan[C]∥Stanley C J et al(eds).Mineral deposits:Processes to processing:Rotterdam,Balkema,1999,2:1375-1378.
[66]陈喜峰,彭润民,刘家军,等.吉尔吉斯斯坦库姆托尔超大型金矿床地质特征[J].黄金,2010,31(12):15-19.
[67]Seltmann R,Jenchuraeva R,eds.Paleozoic geodynamics and gold deposits in the Kyrgyz Tien Shan[M].London,Natural History Museum,IAGOD Guidebook Series,2001,9:182.
[68]彭润民,王建平,刘家军,等.吉尔吉斯斯坦库姆托尔金矿床的叠加成矿特征[J].矿床地质,2012,31(增刊):769-770.
[69]刘家军,郑明华,龙训荣,等.新疆萨瓦亚尔顿金矿床赋矿地层时代的重新厘定及其意义[J].科学通报,1999,44(6):653-656.
[70]叶庆同,吴一平,傅旭杰,等.西南天山金和有色金属矿床成矿条件和成矿预测[M].北京:地质出版社,1999:129-140.
[71]李新生,罗卫东.中国首例穆龙套型金矿——新疆萨瓦亚尔顿金矿地质特征[J].甘肃地质学报,1997,6(1):62-66.
[72]Zhou T,Goldfarb R J,Phillops G N.Tectonics and distribution of gold deposits in China:An overview[J].Mineralium Deposita,2002,37:249-282.
[73]陈富文,李华芹.新疆萨瓦亚尔顿金锑矿床成矿作用同位素地质年代学[J].地球学报,2003,24(6):563-567.
[74]刘家军,郑明华,龙训荣,等.新疆萨瓦亚尔顿金矿床成矿特征及其与穆龙套型金矿床的异同性[J].矿物学报,2002,22(1):54-61.
[75]郑明华,张寿庭,刘家军,等.西南天山穆龙套型金矿床产出地质背景与成矿机制[M].北京:地质出版社,2001:1-131.
[76]董新丰,薛春纪,石福品.新疆西天山大山口金矿地质及成矿流体包裹体地球化学[J].地学前缘,2011,18(5):172-181.
[77]鲍庆忠,王宏,沙德铭,等.新疆和静县大山口金矿床地质特征及其与穆龙套金矿床对比[J].贵金属地质,2000,9(4):200-205.
[78]刘家军,李恩东,龙训荣,等.西南天山大山口金矿床中石英40 Ar-39 Ar快中子活化年龄及其意义[J].吉林大学学报(地球科学版),2004,34(1):37-43.
[79]刘春涌.吉尔吉斯斯坦库姆托尔特大型和塔尔迪布拉克超大型金矿床[J].中亚信息,2005(1):18-20.
[80]刘春涌.吉尔吉斯斯坦的主要金矿床[J].中亚信息.,2004(12):31-34.
[81]王宏,鲍庆忠,沙德铭,等.萨恨托亥金矿床的地球化学异常特征[J].地质与资源,2002(1):23-28.
[82]陈哲夫,周守澐,乌统旦.中亚大型金属矿床特征与成矿环境[M].乌鲁木齐:新疆科技卫生出版社,1999:37-117.
[83]杨建国,闫晔轶,徐学义,等.西南天山成矿规律及其与境外对比研究[J].矿床地质,2004,23(1):20-30.
[84]朱永峰,何国琦,安芳.中亚成矿域核心地区地质演化与成矿规律[J].地质通报,2007,26(9):1167-1177.
[85]郑明华,刘家军,龙训荣,等.西南天山萨瓦亚尔顿金矿床成矿地球化学特征[J].矿物岩石地球化学通报,2000,19(4):226-227.
[86]李福春.穆龙套金矿田地质特征[J].贵金属地质,1996,5(3):228-233.
[87]蔡宏渊,郑跃鹏,李福春,等.穆龙套金矿地质考察[J].矿产与地质,1993,38(7):408-413.
[88]Greenwood P F,Brocks J J,Grice K,et al.Organic geochemistry and mineralogy.I.Characterisation of organic matter associated with metal deposits[J].Ore Geology Reviews,2013,50:1-27.
[89]Kotov N V,Poritskaya L G.The Muruntau gold deposit:Its geologic structure,metasomatic mineral associations and origin[J].International Geology Review,1992,34:77-87.
[90]刘家军,龙训荣,郑明华,等.新疆萨瓦亚尔顿金矿床石英的40 Ar-39 Ar快中子活化年龄及其意义[J].矿物岩石,2002,22(3):19-23.
[91]叶锦华,孟祥金.穆龙套金矿成矿条件与成因模式[C]∥陈毓川,王保良,王安建,等.当代矿床资源勘查与评价的理论与方法,北京:地震出版社,1998:1-560.
[92]孟祥金,叶锦华,王立本.南天山萨恨托亥—大山口一带穆龙套型金矿床地质及地球化学特征[J].地球学报,2000,21(4):379-388.
[93]章振根,马力.甘新交界处的210金矿床与穆龙套金矿床的对比研究[J].黄金科学技术,1994,2(2):9-16.
[94]Southam G.The Geomicrobiology of Ore Deposits[J].Economic Geology,2005,100(6):1067-1084.
[95]Southam G,Saunders J A.The geomicrobiology of ore deposits[J].Economic Geology,2005,100:1067-1084.
[96]庄道泽,杨万志.化探工作在萨瓦亚尔顿金矿发现中的作用[J].新疆地质,1998,16(1):69-75.
[97]施俊法,唐金荣,周平,等.世界找矿模型与矿产勘查[M].北京:地质出版社,2010:1-250.
(1)张招崇,薛春纪,左国朝,等.南天山成矿带对比研究与勘查技术集成项目研究报告[R].北京:国家科技报告服务系统(内部资料),2011.
[2]Porter T M.An overview of the world's porphyry of other hydrothermal Cu and Au deposits and their distribution[J].Porphyry and hydrothermal Cu Au deposits-A global perspective,Conference Proceedings,1998:3-17.
[3]薛春纪,赵晓波,莫宣学,等.西天山“亚洲金腰带”及其动力背景和成矿控制与找矿[J].地学前缘,2014,21(5):128-155.
[4]刘德权,唐延龄,周汝洪.新疆穆龙套型金矿的找矿方向[J].黄金科学技术,1998,6(1):18-23.
[5]戴自希,白冶,吴初国,等.中国西部和毗邻国家铜金找矿潜力的对比研究[M].北京:地震出版社,2001:57-73.
[6]陈哲夫.新疆与邻区南天山超大型金矿成矿条件和找矿方向[J].新疆地质,2002,20(3):229-232.
[7]刘家军,郑明华,龙训荣,等.新疆萨瓦亚尔顿穆龙套型金矿床的确认及其意义[J].贵金属地质,2000,9(3):129-143.
[8]鲍庆中,沙德铭,王宏.也谈南天山古生代造山带内穆龙套型金矿床的控矿因素和找矿方向[J].地质与资源,2003,12(3):159-165.
[9]杨富全,王义天,李蒙文,等.新疆天山黑色岩系型矿床的地质特征及找矿方向[J].地质通报,2005,24(5):462-469.
[10]刘春涌,王永江.初论中亚黑色岩系型金矿床的基本特征——兼论新疆黑色岩系型金矿找矿方向[J].新疆地质,2007,25(1):34-39.
[11]Groves D I,Goldfarb R J,Gebre-Mariam M,et al.Orogenic gold deposits:A proposed classification in the context of their crustal distribution and relationship to other gold deposit types[J].Ore Geology Reviews,1998,13(1):7-27.
[12]Goldfarb R J,Groves D I,Gardoll S.Orogenic gold and geologic time:aglobal synthesis[J].Ore Geology Reviews,2001,18(1):1-75.
[13]Kempe U,Belyatsky B V,Krymsky R S,et al.Sm-Nd and Sr isotope systematics of scheelite from the giant Au(-W)deposit Muruntau(Uzbekistan):implications for the age and sources of Au mineralization[J].Mineralium Deposita,2001,36(5):379-392.
[14]Bierlein F P,Groves D I,Goldfarb R J,et al.Lithospheric controls on the formation of provinces hosting giant orogenic gold deposits[J].Mineralium Deposita,2006,40(8):874-886.
[15]Frimmel H E.Earth's continental crustal gold endowment[J].Earth and Planetary Science Letters,2008,267(1):45-55.
[16]陈华勇,陈衍景,倪培,等.南天山萨瓦亚尔顿金矿流体包裹体研究:矿床成因和勘探意义[J].矿物岩石,2004,24(3):46-54.
[17]陈华勇,陈衍景,倪培,等.新疆萨瓦亚尔顿金矿流体包裹体成分、矿床成因和成矿预测[J].岩石学报,2007,23(9):2189-2197.
[18]薛春纪,赵晓波,莫宣学,等.西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J].地质学报,2014,88(12):2490-2531.
[19]毛景文,韩春明,王义天,等.中亚地区南天山大型金矿带的地质特征、成矿模型和勘查准则[J].地质通报,2002,21(1):858-867.
[20]Mao J,Konopelko D,Seltmann R,et al.Post collisional Age of the Kumtor Gold Deposit and Timing of Hercynian Events in the Tien Shan,Kyrgyzstan[J].Economic Geology,2004,99:1771-1780.
[21]Pasava J,Frimmel H,VymazalováA,et al.A two-stage evolution model for the Amantaytau orogenic-type gold deposit in Uzbekistan[J].Mineralium Deposita,2013,48:825-840.
[22]Liu J,Zheng M,Cook N J,et al.Geological and geochemical characteristics of the Sawaya'erdun gold deposit,southwestern Chinese Tianshan[J].Ore Geology Reviews,2007,32(1):125-156.
[23]杨富全.西南天山金矿成矿条件及成矿机制[D].北京:中国地质科学院,2005:1-186.
[24]Drew L J,Berger B R,Kurbanov N K.Geology and structural evolution of the Muruntau gold deposit,Kyzylkum desert,Uzbekistan[J].Ore Geology Reviews,1996,11(4):175-196.
[25]Graupner T,Kempe U,Spooner E T C,et al.Microthermometric,Laser Raman Spectroscopic,and Volatile-Ion Chromatographic Analysis of Hydrothermal Fluids in the Paleozoic Muruntau Au-Bearing Quartz Vein Ore Field,Uzbekistan[J].Economic Geology,2001,96:1-23.
[26]Wilde A R,Layer P,Mernagh T,et al.The Giant Muruntau Gold Deposit:Geologic,Geochronologic,and Fluid Inclusion Constraints on Ore Genesis[J].Economic Geology,2001,96(3):633-644.
[27]Graupner T,Niedermann S,Kempe U,et al.Origin of ore fluids in the Muruntau gold system:Constraints from noble gas,carbon isotope and halogen data[J].Geochimica et Cosmochimica Acta,2006,70(21):5356-5370.
[28]Morelli R,Creaser R A,Seltmann R,et al.Age and source constraints for the giant Muruntau gold deposit,Uzbekistan,from coupled Re-Os-He isotopes in arsenopyrite[J].Geology,2007,35(9):795-798.
[29]Yang F,Mao J,Wang Y,et al.Geology and Metallogenesis of the Sawayaerdun Gold Deposit in the Southwestern Tianshan Mountains,Xinjiang,China[J].Resource Geology,2007,57(1):57-75.
[30]叶锦华,王立本,叶庆同,等.西南天山萨瓦亚尔顿金(锑)矿床成矿时代与赋矿地层时代[J].地球学报,1999,20(3):278-283.
[31]叶锦华,叶庆同,王进,等.萨瓦亚尔顿金(锑)矿床地质地球化学特征与成矿机理探讨[J].矿床地质,1999,18(1):63-72.
[32]郑明华,刘家军,张寿庭,等.萨瓦亚尔顿金矿床的同位素组成特征及其成因意义[J].成都理工学院学报,2002,11(3):140-146.
[33]杨富全,毛景文,王义天,等.新疆萨瓦亚尔顿金矿床年代学、氦氩碳氧同位素特征及其地质意义[J].地质论评,2006,52(3):341-351.
[34]Chen H Y,Chen Y J,Baker M.Isotopic geochemistry of the Sawayaerdun orogenic-type gold deposit,Tianshan,northwest China:Implications for ore genesis and mineral exploration[J].Chemical Geology,2012,310/311:1-11.
[35]杨富全,叶庆同,傅旭杰,等.新疆西南天山金矿分布、类型和成矿条件[J].新疆地质,1999,17(2):129-136.
[36]杨富全,毛景文,王义天,等.新疆西南天山金矿床主要类型、特征及成矿作用[J].矿床地质,2007,26(4):361-379.
[37]杨在峰,朱志新,王克卓,等.新疆西天山地区黑色岩系金矿成矿地质特征及找矿潜力分析[J].新疆地质,2008,26(3):247-252.
[38]聂凤军,江思宏,侯万荣,等.内蒙古中西部浅变质岩为容矿围岩的金矿床地质特征及形成过程[J].矿床地质,2010,29(1):58-70.
[39]高俊,龙灵利,钱青,等.南天山:晚古生代还是三叠纪碰撞造山带[J].岩石学报,2006,22(5):1049-1061.
[40]Sengor A M C,Natal'in B A.Turkic-type orogeny and its role in the making of the continental crust[J].Annual Reviews of Earth and Planetary Sciences,1996,24:263-337.
[41]Xiao W J,Han C M,Yuan C,et al.Middle Cambrian to Permian subduction-related accretionary orogenesis of Northern Xinjiang,NW China:Implications for the tectonic evolution of central Asia[J].Journal of Asian Earth Science,2008,32:102-117.
[42]Xiao W J,Kr9ner A,Windley B F.Geodynamic evolution of Central Asia in the Paleozoic and Mesozoic[J].International Journal of Earth Sciences,2009,98:1185-1188.
[43]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.
[44]王超,刘良,车自成,等.西南天山阔克萨彦岭巴雷公镁铁质岩石的地球化学特征:LA-ICP-MS U-Pb年龄及其大地构造意义[J].地质论评,2007,53(6):743-754.
[45]Wang B,Shu L S,Faure M,et al.Paleozoic tectonics of the southern Chinese Tianshan:insights from structural,chronological and geochemical studies of the Heiyingshan ophiolitic mélange(NW China)[J].Tectonophysics,2011,497:85-104.
[46]Han B F,He G Q,Wang X C,et al.Late Carboniferous collision between the Tarim and Kazakhstan-Yili terranes in the western segment of the South TianShan Orogen,Central Asia,and implications for the Northern Xinjiang,western China[J].Earth-Science Reviews,2011,109:74-93.
[47]龙灵利,高俊,熊贤明,等.南天山库勒湖蛇绿岩地球化学特征及其年龄[J].岩石学报,2006,22(1):65-73.
[48]马中平,夏林圻,徐学义,等.南天山库勒湖蛇绿岩锆石年龄及其地质意义[J].西北大学学报(自然科学版),2007,37(1):107-110.
[49]张成立,周鼎武,王居里,等.南天山库米什南黄尖石山岩体的年代学、地球化学和Sr、Nd同位素组成及其成因意义[J].岩石学报,2007,23(8):1821-1829.
[50]Mirkamalov R K,Isokov M U,Chirikin V V,et al.New results of U-Pb(SHRIMP)dating of Granitoid and Methamophic complexs of the Tien Shan Folded Belt[C]∥Kbarov Kh A A,Nurtaev B S.Geosciences in Uzbekistan,Tashkent,2012:114-125.
[51]Gao J,Klemd R.Formation of HP-LT rocks and their tectonic implications in the western Tianshan Orogen,NW China:geochemical and age constraints[J].Lithos,2003,66:1-22.
[52]Hegner E,Klemd R,Kr9ner A,et al.Mineralogy ages and P-T conditions of late Paleozoic high-pressure eclogite and provenance of mélange sediments in the South Tianshan Orogen of Kyrgyzstan[J].American Journal of Science,2010,310:916-950.
[53]Su W,Gao J,Klemd R,et al.U-Pb zircon geochronology of Tianshan eclogites in NW China:implication for the collision between the Yili and Tarim blocks of the southwestern Altaids[J].European Journal of Mineralogy,2010,22:473-478.
[54]Li Q L,Lin W,Su W,et al.SIMS U-Pb rutile age of lowtemperature eclogites from southwestern Chinese Tianshan,NW China[J].Lithos,2011,122:76-86.
[55]Klemd R,Br9cker M,Hacker B R,et al.New age constraints on the metamorphic evolution of the high-pressure/low-temperature belt in the western Tianshan Mountains,NWChina[J].Journal of Geology,2005,113:157-168.
[56]Zverev Yu,Kremenetsky A,Minzer E,et al.The Amantaytau—Daughyztau ore field[C]∥Shayakubov T,Islamov F,Kremenetsky A,et al.Au,Ag and Cu deposits of Uzbekistan.Excursion Guidebook,International Field Conference of IGCP-373,Excursion B6of the Joint SGA-IAGOD Symposium,London/Tashkent,1999,27/28,August-4September:17-74.
[57]Wall V J,Yantzen V,Graupner T,et al.Muruntau,Uzbekistan Report on CERCAMS Research Project[R].2004:1-96.
[58]Kostitsyn Y A.Rb-Sr isotopic study of the Muruntau deposit:Magmatism,metamorphism,and mineralization[J]:Geochemistry International,1996,34:1009-1023.
[59]Bagdasaryan A G,Fedyanin A S,Shemetov P A.Estimate of the formation time and other parameters of a disruption structure in open pit walls in terms of Muruntau open pit[J].Journal of Mining Science,2009,45(2):146-151.
[60]谭娟娟,朱永峰.穆龙套金矿地质和地球化学[J].矿物岩石地球化学通报,2008,27(4):391-398.
[61]孟广路,王斌,李宝强,等.乌兹别克斯坦穆龙套金矿床研究进展[J].地质科技情报,2013,32(5):160-166.
[62]Zverev Yu,Kremenetsky A,Minzer E,et al.The Amantaytau—Daughyztau ore field[C]∥Shayakubov T,Islamov F,Kremenetsky A,Seltmann R(eds).Au,Ag,and Cu deposits of Uzbekistan.Excursion guidebook,International Field Conference of IGCP-373,Excursion B6of the Joint SGA-IAGOD Symposium,London/Tashkent,1999,27/28,August–4September:17-35.
[63]Kurbanov N K,Romanov V L,Arifulov C R R,et al.Geological guidebook to the gold deposits of Uzbekistan(for the USGS)[M].Central Research Institute of Geological Prospecting for Base and Precious Meas(TsNIGRI),Moscow,1991:19.
[64]Nikonorov V V,Karaev Y V,Borisov F I,et al.Gold resources of Kyrgyzstan[M].Bishkek,2007:1-500.
[65]Ansdell K M,Abeleira A,Ivanov S.Structural evolution and vein paragenesis at the Kumtor gold deposit,Kyrgyzstan[C]∥Stanley C J et al(eds).Mineral deposits:Processes to processing:Rotterdam,Balkema,1999,2:1375-1378.
[66]陈喜峰,彭润民,刘家军,等.吉尔吉斯斯坦库姆托尔超大型金矿床地质特征[J].黄金,2010,31(12):15-19.
[67]Seltmann R,Jenchuraeva R,eds.Paleozoic geodynamics and gold deposits in the Kyrgyz Tien Shan[M].London,Natural History Museum,IAGOD Guidebook Series,2001,9:182.
[68]彭润民,王建平,刘家军,等.吉尔吉斯斯坦库姆托尔金矿床的叠加成矿特征[J].矿床地质,2012,31(增刊):769-770.
[69]刘家军,郑明华,龙训荣,等.新疆萨瓦亚尔顿金矿床赋矿地层时代的重新厘定及其意义[J].科学通报,1999,44(6):653-656.
[70]叶庆同,吴一平,傅旭杰,等.西南天山金和有色金属矿床成矿条件和成矿预测[M].北京:地质出版社,1999:129-140.
[71]李新生,罗卫东.中国首例穆龙套型金矿——新疆萨瓦亚尔顿金矿地质特征[J].甘肃地质学报,1997,6(1):62-66.
[72]Zhou T,Goldfarb R J,Phillops G N.Tectonics and distribution of gold deposits in China:An overview[J].Mineralium Deposita,2002,37:249-282.
[73]陈富文,李华芹.新疆萨瓦亚尔顿金锑矿床成矿作用同位素地质年代学[J].地球学报,2003,24(6):563-567.
[74]刘家军,郑明华,龙训荣,等.新疆萨瓦亚尔顿金矿床成矿特征及其与穆龙套型金矿床的异同性[J].矿物学报,2002,22(1):54-61.
[75]郑明华,张寿庭,刘家军,等.西南天山穆龙套型金矿床产出地质背景与成矿机制[M].北京:地质出版社,2001:1-131.
[76]董新丰,薛春纪,石福品.新疆西天山大山口金矿地质及成矿流体包裹体地球化学[J].地学前缘,2011,18(5):172-181.
[77]鲍庆忠,王宏,沙德铭,等.新疆和静县大山口金矿床地质特征及其与穆龙套金矿床对比[J].贵金属地质,2000,9(4):200-205.
[78]刘家军,李恩东,龙训荣,等.西南天山大山口金矿床中石英40 Ar-39 Ar快中子活化年龄及其意义[J].吉林大学学报(地球科学版),2004,34(1):37-43.
[79]刘春涌.吉尔吉斯斯坦库姆托尔特大型和塔尔迪布拉克超大型金矿床[J].中亚信息,2005(1):18-20.
[80]刘春涌.吉尔吉斯斯坦的主要金矿床[J].中亚信息.,2004(12):31-34.
[81]王宏,鲍庆忠,沙德铭,等.萨恨托亥金矿床的地球化学异常特征[J].地质与资源,2002(1):23-28.
[82]陈哲夫,周守澐,乌统旦.中亚大型金属矿床特征与成矿环境[M].乌鲁木齐:新疆科技卫生出版社,1999:37-117.
[83]杨建国,闫晔轶,徐学义,等.西南天山成矿规律及其与境外对比研究[J].矿床地质,2004,23(1):20-30.
[84]朱永峰,何国琦,安芳.中亚成矿域核心地区地质演化与成矿规律[J].地质通报,2007,26(9):1167-1177.
[85]郑明华,刘家军,龙训荣,等.西南天山萨瓦亚尔顿金矿床成矿地球化学特征[J].矿物岩石地球化学通报,2000,19(4):226-227.
[86]李福春.穆龙套金矿田地质特征[J].贵金属地质,1996,5(3):228-233.
[87]蔡宏渊,郑跃鹏,李福春,等.穆龙套金矿地质考察[J].矿产与地质,1993,38(7):408-413.
[88]Greenwood P F,Brocks J J,Grice K,et al.Organic geochemistry and mineralogy.I.Characterisation of organic matter associated with metal deposits[J].Ore Geology Reviews,2013,50:1-27.
[89]Kotov N V,Poritskaya L G.The Muruntau gold deposit:Its geologic structure,metasomatic mineral associations and origin[J].International Geology Review,1992,34:77-87.
[90]刘家军,龙训荣,郑明华,等.新疆萨瓦亚尔顿金矿床石英的40 Ar-39 Ar快中子活化年龄及其意义[J].矿物岩石,2002,22(3):19-23.
[91]叶锦华,孟祥金.穆龙套金矿成矿条件与成因模式[C]∥陈毓川,王保良,王安建,等.当代矿床资源勘查与评价的理论与方法,北京:地震出版社,1998:1-560.
[92]孟祥金,叶锦华,王立本.南天山萨恨托亥—大山口一带穆龙套型金矿床地质及地球化学特征[J].地球学报,2000,21(4):379-388.
[93]章振根,马力.甘新交界处的210金矿床与穆龙套金矿床的对比研究[J].黄金科学技术,1994,2(2):9-16.
[94]Southam G.The Geomicrobiology of Ore Deposits[J].Economic Geology,2005,100(6):1067-1084.
[95]Southam G,Saunders J A.The geomicrobiology of ore deposits[J].Economic Geology,2005,100:1067-1084.
[96]庄道泽,杨万志.化探工作在萨瓦亚尔顿金矿发现中的作用[J].新疆地质,1998,16(1):69-75.
[97]施俊法,唐金荣,周平,等.世界找矿模型与矿产勘查[M].北京:地质出版社,2010:1-250.
(1)张招崇,薛春纪,左国朝,等.南天山成矿带对比研究与勘查技术集成项目研究报告[R].北京:国家科技报告服务系统(内部资料),2011.