塔北隆起张性构造带形成机制与油气关系

新疆石油地质 ›› 1997, Vol. 18 ›› Issue (1): 13-17.

塔北隆起张性构造带形成机制与油气关系

刘学锋, 时卫东, 彭德堂, 刘绍平, 钟广法

江汉石油学院湖北江陵 434202

收稿日期:1995-12-09 发布日期:2021-01-18
作者简介:刘学锋,讲师石油地质

FORMING MECHANISM OF TENSIONAL TECTONICS BELT AND THE REL ATION WITH HYDROCARBON IN TABEI UPLIFT

Liu Xuefeng, Shi Weidong, Peng Detang, Liu Shaoping, Zhong Guangfa

Jianghan Petroleum Institute, Jiangling, Hubei 434202

Received:1995-12-09 Published:2021-01-18
About author:Liu Xuefeng,Lecturer, Petroleum Geology

摘要/Abstract

摘要： 塔北隆起张性构造带分布于隆起轴部的轮台断隆上,主要为早期断裂受喜马拉雅运动早期的左旋扭动在浅层派生的北西-南东向张性构造。断裂在平面上呈左行雁列展布,在剖面上为小型地堑组合,部分断裂向深部与先存断裂联合形成负反转构造。与断裂相伴的褶皱构造沿断裂走向分布,且受断裂活动控制。塔北隆起张性构造带位于极有利的构造部位,具有良,好的油气远景。

关键词: 地堑, 断裂, 褶皱, 扭动构造体系, 应力场

Abstract: Tabei uplift tensional tectonics belt distributed in Luntai fault-uplift at its axis, mostly formed in early period of Himalayan event, controlled by the left-lateral couple of force, resulted from NW-SE striking local tensile stress field caused by sinistral torsion of the pre-existing fault in early period of Himalayan orogeny. Faults appear in a left-lateral echelon arrangement in plane and as small-sized graben combination in section. The deeper part of faults formed negative inverted structure along with the pre-existing fault. Fold structure associated with the fault distributed along fault strike, controlled by faulting. Tabei uplift tensional tectonics belt is. expected to have satisfactory oil and gas prospect due to its favorable structural position.

Key words: Graben, Fault, Fold, Shear structural system, Stress field

刘学锋, 时卫东, 彭德堂, 刘绍平, 钟广法. 塔北隆起张性构造带形成机制与油气关系[J]. 新疆石油地质, 1997, 18(1): 13-17.

Liu Xuefeng, Shi Weidong, Peng Detang, Liu Shaoping, Zhong Guangfa. FORMING MECHANISM OF TENSIONAL TECTONICS BELT AND THE REL ATION WITH HYDROCARBON IN TABEI UPLIFT[J]. Xinjiang Petroleum Geology, 1997, 18(1): 13-17.

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