柯坪断隆古生代的构造属性及其演化特征

doi:10.11743/ogg20010406

石油与天然气地质 ›› 2001, Vol. 22 ›› Issue (4): 314-318.doi: 10.11743/ogg20010406

柯坪断隆古生代的构造属性及其演化特征

张臣¹, 郑多明², 李江海¹

1. 北京大学地质学系, 北京, 100871;
2. 塔里木石油勘探开发指挥部, 新疆库尔勒, 841000

收稿日期:2001-09-12 出版日期:2001-12-25 发布日期:2012-01-16
基金资助:
国家自然科学基金资助项目(编号:40072072)

ATTRIBUTE OF PALEOZOIC STRUCTURES AND ITS EVOLUTION CHARACTERISTICS IN KEPING FAULT-UPLIFT

Zhang Chen¹, Zheng Duoming², Li Jianghai¹

1. Department of Geology, Beijing University, Bejing;
2. Tarim Headquarters of Petroleum Exploration and Development, Kurle, Xinjiang

Received:2001-09-12 Online:2001-12-25 Published:2012-01-16

摘要/Abstract

摘要：

柯坪断隆与巴楚隆起古生代无论在地层系统、岩石组合、古生物及沉积相特征等方面均存在可比性,表明柯坪断隆和巴楚隆起前中生代是连为一体的,同属塔里木盆地的组成部分.中生代柯坪巴楚隆起形成雏形,柯坪地区缺失中生代沉积.新生代由于受欧亚板块南缘地体增生,板块碰撞远距离效应和西南天山地区复活造山影响,在上新世末-更新世初,柯坪断隆沿柯坪塔格沙井子断裂发生强烈挤压形成柯坪逆冲推覆构造带.柯坪断隆构成推覆构造带的上部掩冲构造层,巴楚隆起向西北延伸的部分构成推覆构造带的下伏构造层.地面油气显示不能证明地下已无油气藏存在,不能排除在该区找到大型逆冲断层遮挡圈闭型及牵引背斜圈闭型油气藏的可能.

关键词: 构造属性, 逆冲推覆构造, 柯坪断隆

Abstract:

Stratigraphic sequence,rock assemblage,palaeontologic species and sedimentary facies of Palaeozoic Era in Keping region bear comparison with Bachu region.It indicates that Keping and Bachu uplifts were connected in preMesozoic.They were a part of Tarim Basin.Embryonic form of KepingBachu uplift formed in Mesozoic.Mesozoic sediment was lacunae in Keping region.The region was effected by the accretion of southern margin of Eurasian Plate,far distance effect of plate collision and orogeny of southwest Tianshan Mauntains in Cenozoic.Keping thrust belt was formed along Kepingtage Shajingzi fault.Keping uplift constituted the upper thrust nappe of the thrust belt,the northwest extension part of Bachu uplift constituted the underlying structural layer of the thrust belt.It is possible to find oil and gas pools of thrust fault covered trap type and traction fold type.

Key words: structural attribute, thrust nappe, Keping faulted uplift

中图分类号:

P542

张臣,郑多明,李江海. 柯坪断隆古生代的构造属性及其演化特征[J]. 石油与天然气地质, 2001, 22(4): 314-318. doi: 10.11743/ogg20010406 Zhang Chen,Zheng Duoming,Li Jianghai. ATTRIBUTE OF PALEOZOIC STRUCTURES AND ITS EVOLUTION CHARACTERISTICS IN KEPING FAULT-UPLIFT[J]. Oil & Gas Geology, 2001, 22(4): 314-318. doi: 10.11743/ogg20010406

参考文献

[1] Lu Huafu,Jia Dong,Chen Chuming,et al.Evidence for growth fault-bend folds in the Traim basin and its implications for fault-slip rates in the Mesozoic and Cenozoic[J].Proc.30th Int'l.Congr,1996,14:253～262
[2] 卢华复,贾东,蔡东升,等.塔西北柯坪剪切挤压构造[J].高校地质学报,1998,4(1):49～58
[3] 蔡东升,卢华夏,贾东,等.塔里木盆地西北缘柯坪造山带变形分析[A].见:童晓光,梁狄刚,贾承造.塔里木盆地石油地质研究新进展[C].北京:科学出版社,1996.131～138
[4] 汤良杰.塔里木盆地演化和构造样式[M].北京:地质出版社,1996
[5] Yin A,Nie S.Late Cenozoic tectonic evolution of the southern Chinese Tian Shan[J].Tectonics,1998,17(1):1～27
[6] Nishidai T,Berry J L.Structure and hydrocarbon potential of the Tarim basin[J].Journal of Petroleum Geology,1990,13:35～58
[7] 张师本,王成源.从牙形刺动物群论依木干他乌组的时代[J].地层学杂志,1 995,61(1):10～20
[8] 王念忠,张师本.新疆巴楚早志留世软骨鱼类微体化石[J].古脊椎动物学报,1998,36(4):257～267
[9] 王廷印,刘金坤.塔里木盆地成盆期及裂谷作用初探[A].见:贾润胥.中国塔里木盆地北部油气地质研究(第二集):构造与油气[C].武汉:中国地质大学出版社,1991.115～124
[10] 刘金坤,李万茂.塔里木盆地北部玄武岩岩石学特征及其时代归属[A].见:贾润胥.中国塔里木盆地北部油气地质研究(第一集):地层沉积[C].武汉:中国地质大学出版社,1991.194～201
[11] 吕修祥,胡素云.塔里木盆地油气藏形成与分布[M].北京:石油工业出版社,1998.129～136
[12] Mitra S.Duplex structure and imbricate thrust systems:geometry,structural position,and hydrocarbon potential[J].AAPG Bull,1986,70:1 087～1 112
[13] 陈效玉.中国西部盆地边缘(山前)冲断推覆构造与油气聚集[J].石油地质,1994,10(3):263～269

柯坪断隆古生代的构造属性及其演化特征

ATTRIBUTE OF PALEOZOIC STRUCTURES AND ITS EVOLUTION CHARACTERISTICS IN KEPING FAULT-UPLIFT

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 4

编辑推荐

Metrics

[1]	陈石, 郭召杰, 漆家福, 邢向荣. 准噶尔盆地西北缘三期走滑构造及其油气意义[J]. 石油与天然气地质, 2016, 37(3): 322-331.
[2]	管树巍, 杨海军, 韩剑发, 李本亮, 罗春树. 塔中低凸起的构造属性和解释方法[J]. 石油与天然气地质, 2011, 32(5): 777-786.
[3]	孙晓猛, 张梅生, 龙胜祥, 郝福江, 刘鹏举, 刘长垠. 秦岭-大别造山带北部逆冲推覆构造与合肥盆地、周口坳陷控盆断裂[J]. 石油与天然气地质, 2004, 25(2): 191-198.
[4]	陈全茂, 张光亚, 梁晓东, 陈昭年, 周绍强, 王占忠. 张强凹陷及邻区火山岩特征与构造属性[J]. 石油与天然气地质, 1997, 18(4): 309-313.