济阳坳陷沾车地区义东断裂带走滑构造特征及其控藏作用
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  • 英文篇名:Strike-slip structure characteristics of Yidong fault zone and its influence on the hydrocarbon accumulation in Zhanche area,Jiyang Depression
  • 作者:曹默雷 ; 陈书平 ; 刘雅利
  • 英文作者:CAO Molei;CHEN Shuping;LIU Yali;State Key Laboratory of Petroleum Resources and Prospecting,China University of Petroleum(Beijing);Exploration and Development Research Institute,Shengli Oilfield Company,SINOPEC;
  • 关键词:走滑构造特征 ; 控藏作用 ; 义东断裂带 ; 沾车地区 ; 济阳坳陷
  • 英文关键词:strike-slip structure characteristics;;controlling effect on hydrocarbon accumulation;;Yidong fault zone;;Zhanche area;;Jiyang Depression
  • 中文刊名:YQCS
  • 英文刊名:Petroleum Geology and Recovery Efficiency
  • 机构:中国石油大学(北京)油气资源与探测国家重点实验室;中国石化胜利油田分公司勘探开发研究院;
  • 出版日期:2018-09-07 09:18
  • 出版单位:油气地质与采收率
  • 年:2018
  • 期:v.25;No.135
  • 语种:中文;
  • 页:YQCS201806008
  • 页数:5
  • CN:06
  • ISSN:37-1359/TE
  • 分类号:55-59
摘要
济阳坳陷沾车地区义东断裂带走滑构造特征及其控藏作用不明,制约着该区油气勘探。综合地震、测井、钻井等资料开展义东断裂带走滑构造特征分析,并在此基础上评价走滑断裂对油气成藏的控制作用。结果表明:义东断裂走滑特征明显,主断层(义东断层)及其伴生次级断层呈锐角或近直角斜交,平面上呈"入"字型,主断层与两侧的平行断层呈NEE—NE向雁行式展布;剖面上,主断层面陡峭,伴生的次级断层断至主断层面上,形成负花状构造,且具有窄而深的半地堑式构造。义东断裂带控制陡坡带发育多期次、多类型的砂砾岩扇体,断裂多期次活动形成了一系列沿着断层分布的NE向雁列式断块、断鼻及断背斜圈闭,义东断裂主要对油气运移起侧向封堵和垂向输导作用,控制油气沿义东断裂带呈条带状展布。
        The strike-slip structure characteristics of Yidong fault zone and its influence on the hydrocarbon accumulation is unclear in Zhanche area of Jiyang Depression,which restricts the oil and gas exploration in this area. To solve this problem,the strike-slip structure characteristics of Yidong fault zone in Zhanche area were analyzed based on data of seismic,logging and drilling,and the effect of strike-slip faults on hydrocarbon accumulation was evaluated. The result shows that the faults in Yidong fault zone have typical strike-slip characteristics as follows:(1)in the plane,the main fault(F1)is intersected by its associated secondary faults(NWW)with acute or right angle,presenting the shape of"入";while the main fault and its parallel faults in the two sides distribute in NEE-NE direction,presenting an en-echelon form;(2)in the vertical,the main fault has steep fault plane and the associated secondary faults are broken up to showing minus flower structure figure in seismic section,which leads to the formation of narrow and steep half grabens. The Yidong fault zone controls the development of multi-stage and multi-type sandy conglomerate fans and NE-direction distributed fault block,fault nose and fault-related anticline traps. The Yidong fault seals the hydrocarbon laterally but acts as paths for hydrocarbon vertical migration,which results in the belt-like hydrocarbon distribution characteristic along the fault zone.
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