塔里木中新生代盆地扩张和盆地俯冲与地幔柱

高长林; 叶德燎; 张玉箴; 刘光祥

doi:10.11781/sysydz200306661

塔里木中新生代盆地扩张和盆地俯冲与地幔柱

doi: 10.11781/sysydz200306661

中国石化, 石油勘探开发研究院, 无锡实验地质研究所, 江苏, 无锡, 214151

详细信息

作者简介:
高长林(1945- ),男(汉族),江苏泰兴人,博士、教授级高工,主要从事区域地质地球化学和盆地分析研究.

中图分类号: TE121.1
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出版历程
- 收稿日期: 2003-06-17
- 修回日期: 2003-11-10
- 刊出日期: 2003-11-25

EXTENSION AND SUBDUCTION OF THE MESO-CENOZOIC TARIM BASIN AND THEIR RELATIONSHIP WITH MANTLE PLUME

Wuxi Research Institute of Experimental Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

摘要

摘要: 塔里木盆地自二叠纪以来,历经盆地扩张和盆地俯冲以及陆内造山作用的过程.盆地扩张和盆地俯冲是与地幔柱活动相互关联的地质作用,即由于地幔柱的形成和演化,塔里木地区的岩石圈是一个降温过程.早二叠世时,由于热地幔柱上升活动,引起在大陆壳区首先形成巨大的热穹窿构造,再进一步发展演化,形成地堑和断陷盆地.晚二叠世—三叠纪,盆地中部因在早二叠世地幔柱物质喷发后,热上涌减小,再之,由于位于克拉通,地幔岩石圈减薄程度相对较低,古地温较低,达不到产生伸展断陷盆地的临界值,形成陆内坳陷盆地;在盆地边部,由于地幔物质上涌,由盆地中部向四周产生强大的挤压,天山和昆仑山山系快速隆升,向盆地大规模冲断,分别形成两个陆内前陆盆地.侏罗—白垩纪,塔里木地区的岩石圈是一个降温过程,由于热沉降,形成陆内坳陷盆地.新生代,该区经历一个相对较快的降温过程,这一过程对应着大陆聚合、俯冲、逆冲推覆、碰撞造山等各种汇聚—碰撞—挤压环境,由此造成塔里木盆地四周山系不断上升,山系向盆地仰冲,盆地俯冲.正是由于地幔柱的形成和演化,致使盆内扩张,盆边向山内俯冲,发生陆内造山作用.塔里木中新生代的原型盆地有:横张裂陷盆地(早二叠世);陆内前陆盆地和陆内坳陷盆地(晚二叠—三叠纪);陆内坳陷盆地(侏罗—白垩纪);晚期前渊盆地(新生代).
- 中新生代 /
- 盆地扩张 /
- 盆地俯冲 /
- 地幔柱 /
- 塔里木
Abstract: Since the Permian,the Tarim Basin had undergone basinal extension,subduction and intro-continental orogeny.Basinal extension and subduction was related to activity of mantle plume,formation and evolution of mantle plume resulted in geothermal decreasing of lithosphere in the basin.A huge thermal dome structure was firstly formed in continental crust due to rising of hot mantle plume during the Early Permian,and graben and fault basin were further formed.During the Late Permian to Triassic,intra-continental down-warped basin was formed in the central part of the basin as a result of thermal decreasing from mantle after eruption of mantle plume material in the Early Permian;however,strong compression was occurred from centre to outsides because of raising of mantle material,Tianshan and Kunlunshan were fastly uplifted and thrusted towards the basin,and two foreland basins were formed respectively.From the Jurassic to the Cretaceous,it was a thermal decreasing period in the basin,as a result,intra-continental down-warped basin was formed.It was a relative fast period for geothermal decreasing during Cenozoic,which corresponded with continental convergence,subduction,thrust-nappe and collisional orogeny in the area.Mountain system around the basin was uplifted continously and the basin was subducted.Just because of formation and evolution of mantle plume,it resulted in inner basinal extension,subduction and intra-continental orogeny.The protobasin in Meso-Cenozoic includes transverse extensional basin (Early Permian),intra-continental foreland basin and down-warped basin (Late Permian-Triassic),intra-continental down-warped basin (Jurassic-Cretaceous) and late foredeep basin(Cenozoic).
- Meso-Cenozoic /
- basinal extension /
- basinal subduction /
- mantle plume /
- Tarim

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参考文献(38)

[1]	张渝昌,等.中国含油气盆地原型分析[M].南京:南京大学出版社,1997.1-450.
[2]	陈焕疆.论板块大地构造与油气盆地分析[M].上海:同济大学出版社,1990.1-186.
[3]	朱夏,陈焕疆.中国大陆边缘构造和盆地演化[J].石油实验地质,1982,4(3):153-160.
[4]	吉让寿,钱一雄,范小林,等.中国西北地区中生代盆地与油气[M].西安:安地图出版社,2000.1-239.
[5]	朱夏.活动论构造历史观[J].石油实验地质,1991,13(3):201-209.
[6]	朱夏.中国东部板块内部盆地形成机机制的初步探讨[J].石油实验地质,1979(1).
[7]	Zhu X.Chinese sedimentary basins[M].Elsevier Science,1989.1-200.
[8]	孙肇才,邱蕴玉,郭正吾.板内形变与晚期次生成成藏-扬子区海相油气总体形成规律探讨[J].石油实验地质,1991,13(2):107-142.
[9]	冯志强,缪宛芩.南海珠江口盆地的构造演化特征及含油气远景[J].石油实验地质,1982,4(1):19-26.
[10]	吴根耀.盆地研究的活动论构造观[J].石油实验地质,1998,20(4):309-318.
[11]	罗志立.地裂运动与中国油气分布鞋[M].北京:石油工业出版,1992.1-100.
[12]	谢呜谦.拼贴板块构造及其驱动机理[M].北京:科学出版社,2000.1-256.
[13]	张渝昌.关于盆地油气动态成成藏系统研究的理论问题[A].周玉琦,等.朱夏油气地质理论应用研究文集[C].北京:地质出版社,2001,207-220.
[14]	刘光鼎.前新生代海相残留盆地[A].周玉琦,等.朱夏油气地质理论应用研究文集[C].北京:地质出版社,2001,21-23.
[15]	刘金坤,李万茂.塔里木盆地北部玄武岩岩石特征及其时代归属[A].贾润胥.中国塔里木盆地北部油气地质研究[C].武汉:中国地质大学出版社,1991.194-201.
[16]	Whalen J B,Currie K L and Chappell B W.A-type granites:geochemical characteristics,discrimination and petrogenesis[J].Contrib Mineral,1987,95:407-419.
[17]	丁道桂,汤良杰,等.塔里木盆地形成与演化[M].南京:河海大学出版社,1996.1-294.
[18]	高长林,崔可锐,钱一雄,等.天山微板块构造与塔北盆地[M].北京:地质出版社,1995.1-284.
[19]	李佩基,李嵩林,等.中国天山区花岗岩类的演化特征服[J].新疆地质,1985,3(3):50-65.
[20]	周汝洪.新疆同位素地质年代学研究进展出[J].新疆地质,1987,5(4):16-106.
[21]	Graham S A,et al.Collisional successor basins of western China:Impact of tectonic inheritance on land composition[J].Geological Society of America Bulletin,1993,(105):323-344.
[22]	卢华复,陈楚铭,刘志宏,等.库车再生前陆逆冲带的构造特征与成因[J].石油学报,2000,21(3):19-24.
[23]	丁道桂,刘伟新,崔可锐,等.塔里木中新生代前陆盆地构造分析与油气领域[J].石油实验地质,1997,19(2):97-107.
[24]	Molnar P and Chen W P.Evidence of large Cainozoic crustal shortening of Asia[J].Nature,1978,273:218-220.
[25]	Molar P,Tapponnier P.Cenozoic tectonics of Asia:effects of a continental collision[J].Science,1975,189:419-426.
[26]	Tapponnier P,Mercier J L,Proust F.The Tibetan side of the India-Eurasia collision[J].Nature,1981,294:405-410.
[27]	方大钧,金国海,陈汉林.塔里木板块北缘晚古生代、中生代古地磁结果与构造演化的初步探讨[A].贾润胥.中国塔里木盆地北部油气地质研究[C].武汉:中国地质大学出版社,1991.96-104.
[28]	丁道桂,王道轩,刘伟新,等.西昆仑造山带与盆地[M].北京:地质出版社,1996.1-230.
[29]	何登发,李德生.塔里木盆地构造演化与油气聚集[M].北京:地质出版社,1996.1-173.
[30]	白文吉,杨经绥.论大陆盆-山构造格局、盆地扩张及其形成机制[J].长春地质学院学报,1985,(3)49-54.
[31]	汤良杰.塔里木盆地演化和构造样式[M].北京:地质出版社,1996.1-136.
[32]	贾承造,魏国齐,姚慧君,等.盆地构造演化与区域构造地质[M].北京:石油工业出版社,1995.1-174.
[33]	陈发景,汪新文,张光亚,等.塔里木盆地北部构造演化与油气关系[M].北京:地质出版社,1996.1-177.
[34]	康志宏,汤良杰,秦德余.塔里木盆地的原型结构与叠加控油作用[A].张功成,等.中国含油气盆地构造[C].北京:石油工业出版社,1999.233-260.
[35]	徐义刚.地幔柱构造、大火山成岩省及其地质效应[J].地学前缘,2002,9(4):341-354.
[36]	周中毅.塔里木盆地古地温与深部找油(气)前景[J].地球化学,1985,(3):236-241.
[37]	陈荣林,朱宏发,陈跃,等.塔里木盆地中新生界沉积特征与石油地质[M].南京:河海大学出版社,1995.1-118.
[38]	张原庆,钱祥麟,李江海.板块碰撞远程效应的传传播与地球层圈间的运动[J].地学前缘,2001,8(4):341.