塔里木盆地晚奥陶世构造-沉积环境与原型盆地演化
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摘要
塔里木盆地晚奥陶世构造-沉积环境经历了快速而剧烈的变化,恢复该时期盆地原型有助于揭示盆地充填演化和盆山耦合。利用最新的钻井、地震及露头资料以沉积相为研究实体,将盆地充填与周缘构造演化相结合,由点→线→面进行分析,恢复了塔里木盆地晚奥陶世不同时期(以组为单位)的构造-沉积环境,并建立了相应的盆地充填演化和盆山耦合样式。吐木休克组沉积期,塔里木盆地西部发育淹没台地-深水台盆沉积体系,巴楚—塔中和塘南为暴露剥蚀区;良里塔格组沉积期,盆地西部发育开阔台地-深水台盆沉积体系,其中玉北东部—塘古巴斯碳酸盐岩台盆反转为浊流盆地;桑塔木组沉积期,盆地西部发育混积陆棚-浊流盆地沉积体系,仅在柯坪发育欠补偿沉积;铁热克阿瓦提组沉积期,盆地西部广大地区为暴露剥蚀区,并发育碎屑滨岸-陆棚沉积体系。吐木休克组-桑塔木组沉积期,塔里木盆地东部持续发育深水浊流沉积体系;铁热克阿瓦提组沉积期,演变为碎屑陆棚沉积体系。研究认为塔里木盆地晚奥陶世在东西分异的台-盆格局基础上叠加了南北分异的隆-坳格局:吐木休克组沉积期,盆地西部差异升降显著,南北向隆-坳相间的格局初步形成;良里塔格组-桑塔木组沉积期,盆地发生整体的沉降与充填,沉积格局由西厚东薄反转为东厚西薄;铁热克阿瓦提组沉积期,盆地南部和北部发生强烈隆升,古地理格局具南北陆中间海的特征,南北向隆-坳相间的格局定型。在塔里木地块与南部岛弧耦合作用不断加强的背景下,大量陆源碎屑的注入和盆内差异升降作用使得晚奥陶世构造-沉积环境发生了快速变迁。奥陶纪末,在南北双向挤压背景下,大规模的海退和盆内物源区的出现使得塔里木盆地结束了震旦纪以来碳酸盐岩大面积发育的历史,标志着盆地演化进入一个新的阶段。
The tectonic-depositional environment of the Tarim Basin underwent a rapid and dramatic change in the Late Ordovician.The restoration of the proto-type basins has a great significance for the reveal of the basin-mountain coupling and basin fill process.Based on the newest data of drillings,seismic profiles and outcrops,with the analysis of sedimentary facies and the combination of basins and orogenic belts,this paper reconstructed the Late Ordovician tectonic-depositional environment of the Tarim Basin and established the models of basin-mountain couplings and basin fill processes,by employing the method of"point→line→face".In the Tumuxiuke Formation stage,the inundated platform-deep water basin sedimentary system was developed in the western part of the Tarim Basin,and the Bachu-Tazhong area was denudated;In the Lianglitage Formation stage,the open platform-deep water basin sedimentary system was developed and the Yudong-Tanggubasi area underwent the transition from the carbonate basin to the turbidite basin;in the Sangtamu Formation stage,the mixed shelf deposit-turbidite basin sedimentary system was developed and the under-filling deposit was only developed in the Kalpin;In the Tierekeawati Formation stage,the shore-shelf sedimentary system was developed.In the Tumuxiuke Formation-Sangtamu Formation stages,the turbidite basin sedimentary system was continually developed in the eastern part of the Tarim Basin;In the Tierekeawati Formation stage,the clastic shelf sedimentary system was developed in this area.The tectonic-depositional pattern of Tarim Basin in the Late Ordovician had the feature as the following:the platform-basin pattern differentiated from east to west was overlaid with the uplift-depression pattern differentiated from north to south.In the Tumuxiuke Formation stage,the unified platform in the west of the basin had broken down leading to the development of uplift-depression pattern differentiated from north to south.In the Lianglitage Formation-Sangtamu Formation stages,the subsidence and deposition fill occurred overall the basin,the depression died out making the depocenter reversed.In the Tierekeawati Formation stage,the northern and southern part of basin uplifted severely and became land,only the middle part of the basin was covered by water,marking the formation of the uplift-depression pattern differentiated from north to south.Under thebackground that the coupling between basins and orogenic belts increasingly strengthened,the injection of large terrigenous clastics and the up and down of topography made tectonic-depositional environment change rapidly.At the end of the Ordovician,with the sea level descended drastically and the emergence of provenance basin within the basin,the Tarim Basin terminated the history that carbonate sediment grew extensively,signing that basin evolution entered into a new stage.
The tectonic-depositional environment of the Tarim Basin underwent a rapid and dramatic change in the Late Ordovician.The restoration of the proto-type basins has a great significance for the reveal of the basin-mountain coupling and basin fill process.Based on the newest data of drillings,seismic profiles and outcrops,with the analysis of sedimentary facies and the combination of basins and orogenic belts,this paper reconstructed the Late Ordovician tectonic-depositional environment of the Tarim Basin and established the models of basin-mountain couplings and basin fill processes,by employing the method of"point→line→face".In the Tumuxiuke Formation stage,the inundated platform-deep water basin sedimentary system was developed in the western part of the Tarim Basin,and the Bachu-Tazhong area was denudated;In the Lianglitage Formation stage,the open platform-deep water basin sedimentary system was developed and the Yudong-Tanggubasi area underwent the transition from the carbonate basin to the turbidite basin;in the Sangtamu Formation stage,the mixed shelf deposit-turbidite basin sedimentary system was developed and the under-filling deposit was only developed in the Kalpin;In the Tierekeawati Formation stage,the shore-shelf sedimentary system was developed.In the Tumuxiuke Formation-Sangtamu Formation stages,the turbidite basin sedimentary system was continually developed in the eastern part of the Tarim Basin;In the Tierekeawati Formation stage,the clastic shelf sedimentary system was developed in this area.The tectonic-depositional pattern of Tarim Basin in the Late Ordovician had the feature as the following:the platform-basin pattern differentiated from east to west was overlaid with the uplift-depression pattern differentiated from north to south.In the Tumuxiuke Formation stage,the unified platform in the west of the basin had broken down leading to the development of uplift-depression pattern differentiated from north to south.In the Lianglitage Formation-Sangtamu Formation stages,the subsidence and deposition fill occurred overall the basin,the depression died out making the depocenter reversed.In the Tierekeawati Formation stage,the northern and southern part of basin uplifted severely and became land,only the middle part of the basin was covered by water,marking the formation of the uplift-depression pattern differentiated from north to south.Under thebackground that the coupling between basins and orogenic belts increasingly strengthened,the injection of large terrigenous clastics and the up and down of topography made tectonic-depositional environment change rapidly.At the end of the Ordovician,with the sea level descended drastically and the emergence of provenance basin within the basin,the Tarim Basin terminated the history that carbonate sediment grew extensively,signing that basin evolution entered into a new stage.
引文
[1]何治亮,高山林,郑孟林,等.中国西北地区沉积盆地发育的区域构造格局与演化[J].地学前缘,2015,22(3):1-14.
[2]YE H M,LI X H,LI Z X,et al.Age and origin of high BaSr appinite-granites at the northwestern margin of the Tibet Plateau:implications for early Paleozoic tectonic evolution of the Western Kunlun orogenic belt[J].Gondwana Research,2008,13:126-138.
[3]何登发,周新源,张朝军,等.塔里木地区奥陶纪原型盆地类型及其演化[J].科学通报,2007,52(增刊I):126-135.
[4]赵宗举,吴兴宁,潘文庆,等.塔里木盆地奥陶纪层序岩相古地理[J].沉积学报,2009,27(5):939-955.
[5]许志琴,李思田,张建新,等.塔里木地块与古亚洲/特提斯构造体系的对接[J].岩石学报,2011,27(1):1-22.
[6]何登发,周新源,杨海军,等.塔里木盆地克拉通内古隆起的成因机制与构造类型[J].地学前缘,2008,15(2):207-221.
[7]WANG B,SHU L S,MICHEL F,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.
[8]GE R F,ZHU W B,WU H L,et al.The Paleozoic northern margin of the Tarim Craton:passive or active[J].Lithos,2012,142/143:1-15.
[9]LIN C S,YANG H J,LIU J Y,et al.Distribution and erosion of the Paleozoic tectonic unconformities in the Tarim Basin,Northwest China:significance for the evolution of paleouplifts and tectonic geography during deformation[J].Journal of Asian Earth Sciences,2012,46:1-19.
[10]于炳松,林畅松,樊太亮,等.塔里木盆地寒武纪—奥陶纪区域地球动力学转换的沉积作用响应及其储层地质意义[J].地学前缘,2011,18(3):221-232.
[11]张光亚,刘伟,张磊,等.塔里木克拉通寒武纪—奥陶纪原型盆地、岩相古地理与油气[J].地学前缘,2015,22(3):269-276.
[12]冯增昭,鲍志东,吴茂炳,等.塔里木地区奥陶纪岩相古地理[J].古地理学报,2007,9(5):447-460.
[13]林畅松,李思田,刘景彦,等.塔里木盆地古生代重要演化阶段的古构造格局与古地理演化[J].岩石学报,2011,27(1):210-218.
[14]李思田.沉积盆地动力学研究的进展、发展趋向与面临的挑战[J].地学前缘,2015,22(1):1-8.
[15]顾家裕,张兴阳,罗平,等.塔里木盆地奥陶系台地边缘生物礁、滩发育特征[J].石油与天然气地质,2005,26(3):277-283.
[16]张丽娟,李勇,周成刚,等.塔里木盆地奥陶纪岩相古地理特征及礁滩分布[J].石油与天然气地质,2007,28(6):731-737.
[17]焦养泉,荣辉,王瑞,等.塔里木盆地西部一间房露头区奥陶系台缘储层沉积体系分析[J].岩石学报,2011,27(1):285-296.
[18]高达,林畅松,杨海军,等.塔中地区良里塔格组沉积微相及其对有利储层的控制[J].地球科学,2013,38(4):819-831.
[19]钱一雄,沙旭光,李慧莉,等.塔里木盆地塔中西部加里东中、晚期构造-层序结构与奥陶系碳酸盐岩储集体分布[J].地学前缘,2013,20(1):260-274.
[20]刘豪,王英民.塔里木盆地早古生代古地貌-坡折带特征及对地层岩性圈闭的控制[J].石油与天然气地质,2005,26(3):297-304.
[21]许效松,汪正江,万方,等.塔里木盆地早古生代构造古地理演化与烃源岩[J].地学前缘,2005,12(3):49-57.
[22]侯明才,万梨,傅恒.塔河南盐下地区上奥陶统良里塔格组沉积环境分析[J].成都理工大学学报(自然科学版),2006,33(5):509-516.
[23]刘嘉庆,李忠,黄君凑,等.塔里木盆地良里塔格组沉积环境差异及其对碳酸盐储层发育的制约[J].中国科学:地球科学,2012,42(12):1802-1816.
[24]马明侠,陈新军,张学恒.塔里木盆地塔中地区寒武系—奥陶系沉积特征及构造控制[J].石油实验地质,2006,28(6):549-553.
[25]李本亮,管树巍,李传新,等.塔里木盆地塔中低凸起古构造演化与变形特征[J].地质论评,2009,55(4):521-530.
[26]林畅松,杨海军,蔡振中,等.塔里木盆地奥陶纪碳酸盐岩台地的层序结构演化及其对盆地过程的响应[J].沉积学报,2013,31(5):907-919.
[27]贾承造,张师本,吴绍祖.塔里木盆地及周边地层(下册各分区地层表)[M].北京:科学出版社,2004.
[28]王福同,宋志齐,吴绍组.新疆维吾尔族自治区古地理及地质生态图集[CM].北京:中国地图出版社,2006:66-87.
[29]张光亚,刘伟,杨海军.塔里木克拉通寒武纪—奥陶纪原型盆地与岩相古地理[M].北京:科学出版社,2013.
[30]高长林,黄泽光,刘光祥.中国西部古中亚洋与古生代沉积盆地[J].中国西部油气地质,2006,2(2):123-129.
[31]汤良杰,邱海峻,云露,等.塔里木盆地北缘—南天山造山带盆-山耦合和构造转换[J].地学前缘,2012,19(5):195-204.
[32]周肖贝,李江海,王洪浩,等.塔里木盆地南华纪—震旦纪盆地类型及早期成盆构造背景[J].地学前缘,2015,22(3):290-298.
[33]徐向珍,杨经绥,郭国林,等.新疆南天山榆树沟—铜花山蛇绿岩特征和构造背景[J].岩石学报,2011,27(1):96-120.
[34]杨经绥,徐向珍,李天福,等.新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年:早古生代洋盆的证据[J].岩石学报,2011,27(1):77-95.
[35]JIANG T,GAO J,REINER K,et al.Paleozoic ophiolitic mélanges from the South Tianshan Orogen,NW China:geological,geochemical and geochronological implications for the geodynamic setting[J].Tectonophysics,2014,612/613:106-127.
[36]HAN B F,GUO Q H,WANG X C,et al.Late Carboniferous collision between the Tarim and Kazakhstan-Yili terranes in the western segment of the South Tian shan Orogen,Central Asia,and implications for the Northern Xinjiang,Western China[J].Earth-Science Reviews,2011,109(3):74-93.
[37]张斌,陈文,喻顺,等.南天山洋古生代期间俯冲作用过程探讨[J].岩石学报,2014,30(8):2351-2362.
[38]朱志新,李锦秩,董莲慧,等.新疆南天山构造格架及构造演化[J].地质通报,2009,28(12):1864-1870.
[39]王超,罗金海,车自成,等.新疆欧西达坂花岗质岩体地球化学特征和锆石LA-ICP-MS定年:西南天山古生代洋盆俯冲作用过程的启示[J].地质学报,2009,83(2):272-283.
[40]李天福,张建新.西昆仑库地蛇绿岩的二辉辉石岩和玄武岩锆石LA-ICP-MS U-Pb年龄及其意义[J].岩石学报,2014,30(8):2393-2401.
[41]易得功,郑玉壮,弓小平,等.西昆仑库地岩组地质特征及形成时代[J].新疆地质,2013,31(4):281-286.
[42]柳坤峰,王永和,姜高磊,等.西昆仑新元古代—中生代沉积盆地演化[J].地球科学:中国地质大学学报,2014,39(8):987-999.
[43]王超,刘良,何世平,等.西昆仑早古生代岩浆作用过程:布隆花岗岩地球化学和锆石U-Pb-Hf同位素组成研究[J].地质科学,2013,48(4):997-1014.
[44]于晓飞,孙丰月,李碧乐,等.西昆仑大同地区加里东期成岩、成矿事件:来自LA-ICP-MS锆石U-Pb定年和辉钼矿Re-Os定年的证据[J].岩石学报,2011,27(6):1770-1778.
[45]计文化,周辉,李荣社,等.西昆仑新藏公路北段古—中生代多期次构造-热事件年龄确定[J].地球科学:中国地质大学学报,2007,32(5):671-680.
[46]许志琴,杨经绥,张建新,等.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制[J].地质学报,1999,73(3):193-205.
[47]刘永顺,于海峰,辛后田,等.阿尔金山地区构造单元划分和前寒武纪重要地质事件[J].地质通报,2009,28(10):1430-1438.
[48]杨经绥,许志琴,张建新,等.中国主要高压-超高压变质带的大地构造背景及俯冲/折返机制的探讨[J].岩石学报,2009,25(7):1529-1560.
[49]杨经绥,史仁灯,吴才来,等.北阿尔金地区米兰红柳沟蛇绿岩的岩石学特征和SHRIMP定年[J].岩石学报,2008,24(7):1567-1584.
[50]何碧竹,焦存礼,许志琴,等.阿尔金—西昆仑加里东中晚期构造作用在塔里木盆地塘古兹巴斯凹陷中的响应[J].岩石学报,2011,27(11):3435-3448.
[51]刘函,王国灿,杨子江,等.恰什坎萨伊沟玄武岩年代学、地球化学特征及其对比北阿尔金洋盆闭合过程的制约[J].地质学报,2013,87(1):38-54.
[52]董顺利,李忠,高剑,等.阿尔金—祁连—昆仑造山带早古生代构造格架及结晶岩年代学研究进展[J].地质论评,2013,59(4):731-746.
[53]戚学祥,吴才来,李海兵,等.北阿尔金喀孜萨依花岗岩锆石SHRIMP U-Pb定年及其构造意义[J].岩石学报,2005,21(3):859-866.
[54]康磊,刘良,曹玉亭,等.北阿尔金构造带红柳沟钾长花岗岩地球化学特征、LA-ICP-MS锆石U-Pb定年和Hf同位素组成[J].地质通报,2011,30(7):1066-1076.
[55]吴才来,姚尚志,曾令森,等.北阿尔金巴什考供—斯米尔布拉克花岗杂岩特征及锆石SHRIMP U-Pb定年[J].中国科学:D辑,2007,37(1):10-26.
[56]蔡习尧,金仙梅,赵丽娜,等.塔里木盆地上奥陶统良里塔格组划分对比[J].新疆石油地质,2012,33(4):447-449.
[57]陈旭,张元动,李越,等.塔里木盆地及周缘奥陶系黑色岩系的生物地层学对比[J].中国科学:地球科学,2012,42(8):1173-1181.
[2]YE H M,LI X H,LI Z X,et al.Age and origin of high BaSr appinite-granites at the northwestern margin of the Tibet Plateau:implications for early Paleozoic tectonic evolution of the Western Kunlun orogenic belt[J].Gondwana Research,2008,13:126-138.
[3]何登发,周新源,张朝军,等.塔里木地区奥陶纪原型盆地类型及其演化[J].科学通报,2007,52(增刊I):126-135.
[4]赵宗举,吴兴宁,潘文庆,等.塔里木盆地奥陶纪层序岩相古地理[J].沉积学报,2009,27(5):939-955.
[5]许志琴,李思田,张建新,等.塔里木地块与古亚洲/特提斯构造体系的对接[J].岩石学报,2011,27(1):1-22.
[6]何登发,周新源,杨海军,等.塔里木盆地克拉通内古隆起的成因机制与构造类型[J].地学前缘,2008,15(2):207-221.
[7]WANG B,SHU L S,MICHEL F,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.
[8]GE R F,ZHU W B,WU H L,et al.The Paleozoic northern margin of the Tarim Craton:passive or active[J].Lithos,2012,142/143:1-15.
[9]LIN C S,YANG H J,LIU J Y,et al.Distribution and erosion of the Paleozoic tectonic unconformities in the Tarim Basin,Northwest China:significance for the evolution of paleouplifts and tectonic geography during deformation[J].Journal of Asian Earth Sciences,2012,46:1-19.
[10]于炳松,林畅松,樊太亮,等.塔里木盆地寒武纪—奥陶纪区域地球动力学转换的沉积作用响应及其储层地质意义[J].地学前缘,2011,18(3):221-232.
[11]张光亚,刘伟,张磊,等.塔里木克拉通寒武纪—奥陶纪原型盆地、岩相古地理与油气[J].地学前缘,2015,22(3):269-276.
[12]冯增昭,鲍志东,吴茂炳,等.塔里木地区奥陶纪岩相古地理[J].古地理学报,2007,9(5):447-460.
[13]林畅松,李思田,刘景彦,等.塔里木盆地古生代重要演化阶段的古构造格局与古地理演化[J].岩石学报,2011,27(1):210-218.
[14]李思田.沉积盆地动力学研究的进展、发展趋向与面临的挑战[J].地学前缘,2015,22(1):1-8.
[15]顾家裕,张兴阳,罗平,等.塔里木盆地奥陶系台地边缘生物礁、滩发育特征[J].石油与天然气地质,2005,26(3):277-283.
[16]张丽娟,李勇,周成刚,等.塔里木盆地奥陶纪岩相古地理特征及礁滩分布[J].石油与天然气地质,2007,28(6):731-737.
[17]焦养泉,荣辉,王瑞,等.塔里木盆地西部一间房露头区奥陶系台缘储层沉积体系分析[J].岩石学报,2011,27(1):285-296.
[18]高达,林畅松,杨海军,等.塔中地区良里塔格组沉积微相及其对有利储层的控制[J].地球科学,2013,38(4):819-831.
[19]钱一雄,沙旭光,李慧莉,等.塔里木盆地塔中西部加里东中、晚期构造-层序结构与奥陶系碳酸盐岩储集体分布[J].地学前缘,2013,20(1):260-274.
[20]刘豪,王英民.塔里木盆地早古生代古地貌-坡折带特征及对地层岩性圈闭的控制[J].石油与天然气地质,2005,26(3):297-304.
[21]许效松,汪正江,万方,等.塔里木盆地早古生代构造古地理演化与烃源岩[J].地学前缘,2005,12(3):49-57.
[22]侯明才,万梨,傅恒.塔河南盐下地区上奥陶统良里塔格组沉积环境分析[J].成都理工大学学报(自然科学版),2006,33(5):509-516.
[23]刘嘉庆,李忠,黄君凑,等.塔里木盆地良里塔格组沉积环境差异及其对碳酸盐储层发育的制约[J].中国科学:地球科学,2012,42(12):1802-1816.
[24]马明侠,陈新军,张学恒.塔里木盆地塔中地区寒武系—奥陶系沉积特征及构造控制[J].石油实验地质,2006,28(6):549-553.
[25]李本亮,管树巍,李传新,等.塔里木盆地塔中低凸起古构造演化与变形特征[J].地质论评,2009,55(4):521-530.
[26]林畅松,杨海军,蔡振中,等.塔里木盆地奥陶纪碳酸盐岩台地的层序结构演化及其对盆地过程的响应[J].沉积学报,2013,31(5):907-919.
[27]贾承造,张师本,吴绍祖.塔里木盆地及周边地层(下册各分区地层表)[M].北京:科学出版社,2004.
[28]王福同,宋志齐,吴绍组.新疆维吾尔族自治区古地理及地质生态图集[CM].北京:中国地图出版社,2006:66-87.
[29]张光亚,刘伟,杨海军.塔里木克拉通寒武纪—奥陶纪原型盆地与岩相古地理[M].北京:科学出版社,2013.
[30]高长林,黄泽光,刘光祥.中国西部古中亚洋与古生代沉积盆地[J].中国西部油气地质,2006,2(2):123-129.
[31]汤良杰,邱海峻,云露,等.塔里木盆地北缘—南天山造山带盆-山耦合和构造转换[J].地学前缘,2012,19(5):195-204.
[32]周肖贝,李江海,王洪浩,等.塔里木盆地南华纪—震旦纪盆地类型及早期成盆构造背景[J].地学前缘,2015,22(3):290-298.
[33]徐向珍,杨经绥,郭国林,等.新疆南天山榆树沟—铜花山蛇绿岩特征和构造背景[J].岩石学报,2011,27(1):96-120.
[34]杨经绥,徐向珍,李天福,等.新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年:早古生代洋盆的证据[J].岩石学报,2011,27(1):77-95.
[35]JIANG T,GAO J,REINER K,et al.Paleozoic ophiolitic mélanges from the South Tianshan Orogen,NW China:geological,geochemical and geochronological implications for the geodynamic setting[J].Tectonophysics,2014,612/613:106-127.
[36]HAN B F,GUO Q H,WANG X C,et al.Late Carboniferous collision between the Tarim and Kazakhstan-Yili terranes in the western segment of the South Tian shan Orogen,Central Asia,and implications for the Northern Xinjiang,Western China[J].Earth-Science Reviews,2011,109(3):74-93.
[37]张斌,陈文,喻顺,等.南天山洋古生代期间俯冲作用过程探讨[J].岩石学报,2014,30(8):2351-2362.
[38]朱志新,李锦秩,董莲慧,等.新疆南天山构造格架及构造演化[J].地质通报,2009,28(12):1864-1870.
[39]王超,罗金海,车自成,等.新疆欧西达坂花岗质岩体地球化学特征和锆石LA-ICP-MS定年:西南天山古生代洋盆俯冲作用过程的启示[J].地质学报,2009,83(2):272-283.
[40]李天福,张建新.西昆仑库地蛇绿岩的二辉辉石岩和玄武岩锆石LA-ICP-MS U-Pb年龄及其意义[J].岩石学报,2014,30(8):2393-2401.
[41]易得功,郑玉壮,弓小平,等.西昆仑库地岩组地质特征及形成时代[J].新疆地质,2013,31(4):281-286.
[42]柳坤峰,王永和,姜高磊,等.西昆仑新元古代—中生代沉积盆地演化[J].地球科学:中国地质大学学报,2014,39(8):987-999.
[43]王超,刘良,何世平,等.西昆仑早古生代岩浆作用过程:布隆花岗岩地球化学和锆石U-Pb-Hf同位素组成研究[J].地质科学,2013,48(4):997-1014.
[44]于晓飞,孙丰月,李碧乐,等.西昆仑大同地区加里东期成岩、成矿事件:来自LA-ICP-MS锆石U-Pb定年和辉钼矿Re-Os定年的证据[J].岩石学报,2011,27(6):1770-1778.
[45]计文化,周辉,李荣社,等.西昆仑新藏公路北段古—中生代多期次构造-热事件年龄确定[J].地球科学:中国地质大学学报,2007,32(5):671-680.
[46]许志琴,杨经绥,张建新,等.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制[J].地质学报,1999,73(3):193-205.
[47]刘永顺,于海峰,辛后田,等.阿尔金山地区构造单元划分和前寒武纪重要地质事件[J].地质通报,2009,28(10):1430-1438.
[48]杨经绥,许志琴,张建新,等.中国主要高压-超高压变质带的大地构造背景及俯冲/折返机制的探讨[J].岩石学报,2009,25(7):1529-1560.
[49]杨经绥,史仁灯,吴才来,等.北阿尔金地区米兰红柳沟蛇绿岩的岩石学特征和SHRIMP定年[J].岩石学报,2008,24(7):1567-1584.
[50]何碧竹,焦存礼,许志琴,等.阿尔金—西昆仑加里东中晚期构造作用在塔里木盆地塘古兹巴斯凹陷中的响应[J].岩石学报,2011,27(11):3435-3448.
[51]刘函,王国灿,杨子江,等.恰什坎萨伊沟玄武岩年代学、地球化学特征及其对比北阿尔金洋盆闭合过程的制约[J].地质学报,2013,87(1):38-54.
[52]董顺利,李忠,高剑,等.阿尔金—祁连—昆仑造山带早古生代构造格架及结晶岩年代学研究进展[J].地质论评,2013,59(4):731-746.
[53]戚学祥,吴才来,李海兵,等.北阿尔金喀孜萨依花岗岩锆石SHRIMP U-Pb定年及其构造意义[J].岩石学报,2005,21(3):859-866.
[54]康磊,刘良,曹玉亭,等.北阿尔金构造带红柳沟钾长花岗岩地球化学特征、LA-ICP-MS锆石U-Pb定年和Hf同位素组成[J].地质通报,2011,30(7):1066-1076.
[55]吴才来,姚尚志,曾令森,等.北阿尔金巴什考供—斯米尔布拉克花岗杂岩特征及锆石SHRIMP U-Pb定年[J].中国科学:D辑,2007,37(1):10-26.
[56]蔡习尧,金仙梅,赵丽娜,等.塔里木盆地上奥陶统良里塔格组划分对比[J].新疆石油地质,2012,33(4):447-449.
[57]陈旭,张元动,李越,等.塔里木盆地及周缘奥陶系黑色岩系的生物地层学对比[J].中国科学:地球科学,2012,42(8):1173-1181.