塔里木盆地孔雀河地区构造特征

新疆石油地质 ›› 2005, Vol. 26 ›› Issue (6): 627-631.

塔里木盆地孔雀河地区构造特征

田纳新^1,2, 于明德², 涂志民², 马玉春³

1.中国地质大学（北京）,北京 100083;
2.中国石化河南油田分公司勘探开发研究院,河南南阳 473132;
3.中国石化石油勘探开发科学研究院西部分院,乌鲁木齐 830011

收稿日期:2005-04-29 出版日期:2005-12-01 发布日期:2020-11-23
作者简介:田纳新(1968-),男,河南南阳人,高级工程师,在读博士研究生,石油地质,(Tel)0996-8768419.

The Structural Features of Kongquehe Area in Tarim Basin

TIAN Na-xin^1,2, YU Ming-de², TU Zhi-min², MA Yu-chun³

1. China University of Geosciences, Beijing 100083, China;
2. Research Institute of Exploration and Development, Henan Oilfield Company, Sinopec, Nanyang, Henan 473132, China;
3. West Institute, Research Institute of Petroleum Exploration and development, Sinopec, Urumqi, Xinjiang 830011, China

Received:2005-04-29 Online:2005-12-01 Published:2020-11-23

摘要/Abstract

摘要： 孔雀河地区受库鲁克塔格断隆与多期构造运动的影响,构造较为复杂。对该区有重要影响的断裂有孔雀河断裂、巴里英断裂、尉犁断裂和维马克– 开屏断裂。本区经历了 5 个演化阶段:被动陆缘盆地阶段; 挤压反转古鼻凸形成阶段; 克拉通内凹陷阶段; 克拉通内坳陷盆地发展阶段和类前陆盆地发展阶段。加里东末期的构造运动,奠定了下古生界的基本构造轮廓; 燕山运动古生代构造再生; 侏罗系构造基本定型; 喜马拉雅运动使本区发育为类前陆盆地。古生界发育大型鼻凸,中生界以断背斜圈闭为主,依附于逆冲断裂。圈闭类型可划分为 4 大类、10 小类,主要发育 3 种构造样式。

关键词: 孔雀河地区, 变形特征, 构造分区, 构造演化, 构造样式

Abstract: The structural features are complicated in Kongquehe area because of the influences of Kuluktag faulted uplift and multi-stage tectonic movements.The faults that affect the area most are Kongquehe fracture, Baliying fracture, Weili fracture and Weimake-Kaiping fracture.The area had undergone such evolution stages as passive borderland basining, squeeze-retrograde nose-like swelling, cratonic inner sagging, intracratonic basining and para-foreland basin.Late Caledonian tectonic movement formed the basic structural configuration of the Lower Paleozoic; Yanshan movement regenerated Palaeozoic structures and shaped Jurassic structures; Himalayan movement made the area developed as a para-foreland basin.Large-scale nose-like swells were developed during the Palaeozoic era, while the Mesozoic was dominated by the faulted-anticline traps with thrust belt.The trap can be divided into four types and subdivided into ten kinds, and three structural styles were developed in this area.

Key words: Kongquehe area, deformation feature, structural zonation, structural evolvement, structural style

中图分类号:

TE111.2

田纳新, 于明德, 涂志民, 马玉春. 塔里木盆地孔雀河地区构造特征[J]. 新疆石油地质, 2005, 26(6): 627-631.

TIAN Na-xin, YU Ming-de, TU Zhi-min, MA Yu-chun. The Structural Features of Kongquehe Area in Tarim Basin[J]. Xinjiang Petroleum Geology, 2005, 26(6): 627-631.

参考文献

[1] 成守德,王元龙.新疆大地构造演化基本特征[J].新疆地质,1998,16(2):97-107.
[2] 李永安,孙东江,郑洁,等.新疆塔里木及周边古地磁研究与盆地形成演化的探讨[A].新疆第三届天山地质矿产学术讨论会论文选集[C].乌鲁木齐:新疆人民出版社,1995.119-132.
[3] 吴国干,李华其,初宝杰,等.塔里木盆地东部大地构造演化与油气成藏[J].大地构造与成矿学,2002,26(3):229-234.
[4] 吴国干,夏斌,王核,等.塔东地区构造变形特征及其分区[J].新疆地质,2003,21(4):407-411.
[5] 顾家裕,周经才,阎火.塔里木盆地沉积相与油气[M].北京:石油工业出版社,1994.
[6] 谢晓安,吴奇之,卢华复.塔里木盆地古生代构造格架与沉积特征[J].沉积学报,1997,15(1):152-155.
[7] 黄传波.塔里木盆地寒武– 奥陶系碳酸盐岩油气藏形成条件[J].新疆石油地质,2000,21(3):188-192.
[8] 张克银,邵志兵,邹元荣.塔里木盆地孔雀河地区复式油气系统[J].新疆石油地质,2004,25(2):122-124.
[9] 李永林,乔桂林,姚亚明,等.孔雀1 井天然气成因初探[J].河南石油,2003,17(3):4-6.
[10] 严永新,田云,袁光喜,等:孔雀河斜坡含油系统及有利地带[J].新疆石油地质,2003,24(5):411-414.
[11] 杨瑞财,高伟中,杨彩虹,等.塔里木盆地英吉苏凹陷中生界油气勘探潜力[J].新疆石油地质,2000,21(3):184-187.
[12] 林学庆,李永林,李亚玉,等.孔雀河地区油气勘探有利目标[J].新疆石油地质,2003,24(5):427-430.
[13] 邱荣华,李永林.塔里木盆地孔雀河区块石油地质条件与勘探前景[J].河南石油,2003,17(1):1-5.
[14] 李小军,李景明.塔里木盆地东部盆山耦合与区带分析[J].现代地质,2004,18(2):164-169.
[15] 赵增录,刘文汇,杨斌宜,等.孔雀河斜坡维马 2 号(孔雀1井)气藏形成机理[J].新疆石油地质,2003,24(6):549-551.
[16] 梁慧社,刘和甫.新疆塔里木盆地构造样式研究[J].河北地质学院学报,1996,19(3-4):268-276.
[17] 汤良杰.塔里木盆地演化和构造样式[M].北京:地质出版社,1996.41-73.
[18] 贾承造.塔里木盆地构造特征与油气聚集规律[J].新疆石油地质,1999,20(3):177-183.