天然气地质学

塔里木盆地北部隆起牙哈构造带断裂特征

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  • (中国石油塔里木油田公司勘探开发研究院,新疆 库尔勒 841000)
李国会(1974-),男,吉林农安人,工程师,主要从事石油物探工作.

收稿日期: 2007-08-15

  修回日期: 2007-10-12

  网络出版日期: 2008-06-20

CHARACTERISTICS OF FAULT SYSTEM IN YAHA STRUCTURE BELTOF NORTHERN UPLIFT, TARIM BASIN

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  • (Research Institute of Exploration and Development, PetroChina Tarim Oilfield Company, Korla 841000, China)

Received date: 2007-08-15

  Revised date: 2007-10-12

  Online published: 2008-06-20

摘要

牙哈断裂构造带位于塔里木盆地塔北隆起轮台断隆的中段北缘,受多期次构造运动影响该带内断裂异常发育,并且是控制寒武系白云岩裂缝型储集层发育的最主要因素,同时也是该带油气运移的主要通道。通过对断裂的精细刻画、对断裂系统的空间展布和断裂发育史的分析,对该带油气成藏规律和寒武系潜山勘探问题有了进一步的认识。

本文引用格式

李国会;郑多明;王超;韩利军;王兴军 . 塔里木盆地北部隆起牙哈构造带断裂特征[J]. 天然气地球科学, 2007 , 18(6) : 859 -863 . DOI: 10.11764/j.issn.1672-1926.2007.06.859

Abstract

The Yaha fault structure belt is located in the north of the central Luntai anticline of the northern uplift of Tarim basin. Influenced by several tectonic movements, faults are widely developed and fault system is the most important factor that controls the development of Cambrian dolomite fracture reservoirs. In this paper, we analyze the developing time, space distribution and evolution history of the fault system which will contribute to oil and gas accumulation research and exploration of the Cambrian buried hill in this area.

参考文献

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