THE FEATURES OF THE NNE TRENDING FAULTS AND ITS IMPLICATION FOR HYDROCARBON IN THE ZHUANGHAI AREA, BOHAIWAN BASIN

Expand
  • 1. Geophysical Research Institute of Shengli Oilfield Company Limited, Dongying 257003, China;
    2. Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

Received date: 2004-04-19

  Revised date: 2004-07-19

  Online published: 2004-10-20

Abstract

Based on the analysis of high-resoulution 3D seismic data and drilling wells, this paper studies the NNE trending fault and associated structures. The NNE trending faults show an echolon arrangement on horizontal. The different tectonic deformation and strata units exist in the both side of the fault zone. The NNE fault has associated folds by the side of the fault zone. The faults are characterized by flower structure on the seismic profiles. Therefore, the faults have strike-slip movement. The NNE trending faults, which parallel to the Tanlu fault, were possible formed during Indo-China movement. It was active as a right strike-slip fault during Late Jurassic and Early Cretaceous. It controlled the Magan ejection and development of Late Mesozoic sedimentary basin. The faults express as normal fault by right strike-slips movement during Censozoic except tectonic inversion.

Cite this article

ZOU Dong-bo, WU Shi-guo,LIU Gang,HAN Wen-gong . THE FEATURES OF THE NNE TRENDING FAULTS AND ITS IMPLICATION FOR HYDROCARBON IN THE ZHUANGHAI AREA, BOHAIWAN BASIN[J]. Natural Gas Geoscience, 2004 , 15(5) : 503 -507 . DOI: 10.11764/j.issn.1672-1926.2004.05.503

References

[1]Xu J, Zhu G, Tong W X,et al.Formation and evolution of the Tancheng-Lujiang wrench fault system: A major shear system to the north of the Pacific Ocean[J].Tectonophysics, 1997, 134: 273-310.
[2] Zhang Y Q, Dong S W, Shi W. Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province, eastern China[J].Tectonophysics,2003,363: 243-258.
[3] 朱光,牛漫兰,刘国生,等.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件[J].地质学报,2002,76(3):325-334.
[4] 李丕龙,张善文,王永诗,等.多样性潜山成因、成藏与勘探——以济阳坳陷为例[M].北京:石油工业出版社,2003.
[5]谭明友,刘福贵,董臣强,等.埕北30潜山构造演化与油气富集规律研究[J].石油地球物理勘探,2002,37(2):134-138.
[6]刘福贵,谭明友,邴进营,等沾化凹陷东部中、古生界成藏条件及勘探目标研究[A]潘元林.油气地质地球物理综合勘探技术[C].北京:地质出版社,1998. 144-173.
[7]宗国洪,施央申,王秉海,等 .济阳盆地中生代构造特征与油气[J]地质论评,1998,44(3):289-294.
[8]林会喜,王永诗,陈广军,等.埕岛地区古生界潜山油藏地质特征及储层预测[A].潘元林.中国隐蔽油气藏[C].北京:地质出版社,1996.228-240.
[9]谭明友,邴进营.山东北部滨海地区负反转断层及古生界负反转结构成因分析[J]石油地球物理勘探,1996,31(6):844-850.
[10]Harding T P. Petroleum traps associated with wrench faults[J]. AAPG Bull, 1974,57: 97-166.
[11]李晓清,王泽成,程有义,等.拉分盆地分析与含油气性[M].北京:石油大学出版社,2003.
[12]谯汉生,纪友亮,姜再兴.中国东部大陆裂谷盆地与油气[M].北京:石油工业出版社,2003.

Outlines

/