ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
东营河125断层几何学特征及其对浊积扇和油藏的控制作用
  
关键词:arc-fan coincidence  arcuate fault  turbidite fan, geometric characteristic  He 125 fault
基金项目:中国石油天然气集团公司资助项目
作者单位
王志坤 中国石油大学,山东东营257061 
钟建华 中国石油大学,山东东营257061
中国科学院广州地球化学研究所,广东广州510640 
艾合买提江·阿布都热合曼 中国石油大学,山东东营257061 
高玉飞 中国石油大学,山东东营257061 
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摘要:
Geometric Characteristics of the He-125 Fault and Its Control over Sediment and Reservoir Distribution, Dongying
      Based on researches on characteristics of the He125 fault,the authors have found that the arcuate fault is parallel to the fault strike and is the combination of fault-trough and fault-ridge,as evidenced from the profile.In the cross section,the fault can be divided into three parts,namely,vertical-slip part,dip-slip part and horizontal-slip part.A comparison of their growth indices shows that the arc center is greater than the arc flank,but things are just the opposite for their fault dip.There exists some relationship between the geometric features of the fault and its kinematic characteristics.Different geometric characteristics of different localities show the difference of their kinematic characteristics.Geometric features of the fault system control the distribution of sediments.Viewed from the surface,the arc center is the counterpart of the turbidite fan,the arc flank is the boundary of the turbidite fans,the fault trough is the recharge path of the turbidite fan,and the fault ridge is the watershed line of different recharge areas.Viewed from the cross section,the lower dip-slip part corresponds to far-bank turbidite,and its middle and upper part corresponds to the slump turbidite fan,thus forming a typical corresponding phenomenon for the arc and fan.The fault characteristics also play an important role in migration pathway and hydrocarbon accumulation.
WANG Zhi-kun,ZHONG Jian-hua,AHMATJAN·Abdurahman,GAO Yu-fei.2008.Geometric Characteristics of the He-125 Fault and Its Control over Sediment and Reservoir Distribution, Dongying[J].Acta Geoscientica Sinica,29(1):95-102.
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