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周口坳陷谭庄-沈丘凹陷下白垩统断裂特征分析

Featura Analysis of Early Cretaceous Faults of Tanzhuang-Shenqiu Sag in Zhoukou Depression

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【作者】 彭晓波高日胜胡小强

【Author】 PENG Xiao-bo1,GAO Ri-sheng2,HU Xiao-qiang3(1.Key Laboratory of Exploration Technologies for Oil and Gas Resources,Ministry of Education,Yangtze University,Jingzhou 434023,China;2.Petrochina Research Institute of Petroleum Exploration & Development,Beijing 100083,China;3.Guangzhou Marine Geological Survey Bureau,Guangzhou 510760,China)

【机构】 长江大学油气资源与勘探技术教育部实验室中国石油勘探开发研究院广州海洋地质调查局

【摘要】 根据谭庄-沈丘凹陷的地震剖面、钻井资料和区域地质资料,分析了下白垩统断裂的发育和活动特征。按照走向可划分为3组,NWW-NW向、NNE-EW向及近SN向断裂系统。叶鲁断裂和商水断裂分别是谭庄-沈丘凹陷南、北边界的主控断裂,控制着凹陷内下白垩统和新生界的沉积与保存。主要有4期断裂活动:晚侏罗世-早白垩世巴村期-永丰早期断裂活动期;早白垩世末期断裂活动期;新近纪断裂活动期;古近纪断裂活动期。

【Abstract】 Based on seismic profile,drilling data and regional geologieal data,the fault feature of early Cretaceous Faults in Tanzhuang-Shenqiu Sag is analyzed.According to directions of fault,can be divided into NWW-NW,NNE-EW and close to the SN.YeLu fracture and ShangShui fracture were basin-bounding master fault of TanZhuang-ShenQiu Sag.,controls within the early cretaceous and Cenozoic sedimentary and preservation.There are four main fault activity: late Jurassic period of early creatceous;The end of early cretaceous,Neogene,Paleogene.

  • 【分类号】P542.3
  • 【被引频次】2
  • 【下载频次】101
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