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塔里木盆地塔中北坡走滑断裂特征与奥陶系油气勘探

邱华标 印婷 曹自成 韩俊 黄诚 魏华动 刘子豪

海相油气地质2017,Vol.22Issue(4):44-52,9.
海相油气地质2017,Vol.22Issue(4):44-52,9.DOI:10.3969/j.issn.1672-9854.2017.04.006

塔里木盆地塔中北坡走滑断裂特征与奥陶系油气勘探

Strike-slip Fault and Ordovician Petroleum Exploration in Northern Slope of Tazhong Uplift, Tarim Basin

邱华标 1印婷 1曹自成 1韩俊 1黄诚 1魏华动 1刘子豪2

作者信息

  • 1. 中国石化西北油田分公司勘探开发研究院
  • 2. 中国石油东方地球物理勘探有限责任公司
  • 折叠

摘要

Abstract

Based on the structural interpretation and the analysis of 2 D/3D seismic data,it is identified that NE-trending/NEE-trending strike-slip fault zones are distributed in northern slope of Tazhong Uplift, and six identification marks of strike-slip fault in seismic slices and sections are summarized. Three types of strike-slip fault system which superimposed in space are developed, including compresso-shear faults(end of Middle Ordovician to Silurian),tenso-shear faults (Late Devonian to Early Carboniferous) and thrust faults(Late Permian). It is concluded that the development of fractured reservoir and fractured-vuggy reservoir was controled by the intensity of fault deformation,and the development of high-quality fractured-vuggy reservoir was dominated by the segmentation of strike-slip faults. It is suggested that the fracture zones with strong deformation, the pull-apart structure, and the trough fault zone where superimposed reformation by later faults and with beading seismic anomalies are favorable targets for exploring large-scale natural gas reservoir of Ordovician.

关键词

走滑断裂/断裂特征/变形强度/缝洞型储层/奥陶系/塔中北坡/塔里木盆地

Key words

Strike-slip fault/Fault characteristics/Deformation intensity/Fractured-vuggy reservoir/Ordovician/Tazhong Uplift/Tarim Basin

分类

能源科技

引用本文复制引用

邱华标,印婷,曹自成,韩俊,黄诚,魏华动,刘子豪..塔里木盆地塔中北坡走滑断裂特征与奥陶系油气勘探[J].海相油气地质,2017,22(4):44-52,9.

基金项目

本文受国家重大科技专项 "塔里木盆地中央隆起区海相碳酸盐岩层系油气成藏主控因素与勘探突破目标评价"(编号:2011ZX05005-004)资助 (编号:2011ZX05005-004)

海相油气地质

OA北大核心CSCDCSTPCD

1672-9854

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