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二连盆地赛汉塔拉凹陷断裂的生长演化特征

何洪春 龙伟 李应 屈晓艳 杨渊宇 应文峰 杭文艳 李忠权

成都理工大学学报(自然科学版)2016,Vol.43Issue(2):249-256,8.
成都理工大学学报(自然科学版)2016,Vol.43Issue(2):249-256,8.DOI:10.3969/j.issn.1671-9727.2016.02.12

二连盆地赛汉塔拉凹陷断裂的生长演化特征

Growth and evolution characteristics of faults in the Saihantala sag of Erlian Basin,China

何洪春 1龙伟 1李应 2屈晓艳 3杨渊宇 4应文峰 1杭文艳 5李忠权1

作者信息

  • 1. 国土资源部构造成矿成藏重点实验室 成都理工大学,成都 610059
  • 2. 密苏里科技大学 地质与地球物理学院,美国 615401
  • 3. 中国建筑材料工业地质勘查中心 四川总队,成都 610052
  • 4. 中国石油西南油气田分公司 川西北气矿,四川 江油 621700
  • 5. 中国石油西南油气田分公司 成都 610041
  • 折叠

摘要

Abstract

Based on the seismic data,sedimentary pattern analysis,maximum displacement-length fitting diagram and displacement-distance evolution profile,the evolution of fault and its control on oil-gas in Saihantala sag are studied.It reveals that the growth of the boundary fault experienced following stages:(1)During the sedimentary period of Aershan Formation,it could be divided into 3 segments with independent growth;(2 )During the sedimentary period of first Member of Tenger Formation,the south and mid segment linked together;(3)During the sedimentary period of second Member of Tenger Formation,the three segments grows into a whole fault.The second class faults occurred as echelon shapes,formed a typical segment linkage mode in the plane.The growth and evolution experience independent growth stage, soft connection and flexible connection stage respectively.The transfer zone formed in the process of fault growth and segment linkage results in high-quality reservoir rock,with corresponding source rock,cap rock and trap,eventually creating favorable hydrocarbon accumulation.

关键词

断裂/生长演化/油气聚集/赛汉塔拉凹陷/二连盆地

Key words

fault/growth and evolution/hydrocarbon accumulation/Saihantala sag/Erlian Basin

分类

地质学

引用本文复制引用

何洪春,龙伟,李应,屈晓艳,杨渊宇,应文峰,杭文艳,李忠权..二连盆地赛汉塔拉凹陷断裂的生长演化特征[J].成都理工大学学报(自然科学版),2016,43(2):249-256,8.

基金项目

国家自然科学重点基金项目(41030426);国家自然基金主任基金项目(41340004);国家重大专项(2011ZX05004-005-01);四川省科技支撑计划项目(2015SZ0224,2015RZ0032)。 ()

成都理工大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1671-9727

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