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Volume 22 Issue 3
Jun 2011
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Article Contents
Jiahao Wang, Honghan Chen, Hua Wang, Tao Jiang, Hongbo Miao. Two Types of Strike-slip and Transtensional Intrabasinal Structures Controlling Sandbodies in Yitong Graben. Journal of Earth Science, 2011, 22(3): 316-325. doi: 10.1007/s12583-011-0184-7
Citation: Jiahao Wang, Honghan Chen, Hua Wang, Tao Jiang, Hongbo Miao. Two Types of Strike-slip and Transtensional Intrabasinal Structures Controlling Sandbodies in Yitong Graben. Journal of Earth Science, 2011, 22(3): 316-325. doi: 10.1007/s12583-011-0184-7

Two Types of Strike-slip and Transtensional Intrabasinal Structures Controlling Sandbodies in Yitong Graben

doi: 10.1007/s12583-011-0184-7
Funds:

the National Natural Science Foundation of China 40872077

More Information
  • Corresponding author: Wang Jiahao, cugwangjiahao@163.com
  • Received Date: 22 Jun 2009
  • Accepted Date: 10 Dec 2009
  • Publish Date: 01 Jun 2011
  • Recently, the researches on structure controls on sandbodies have provided a new method for predicting petroleum reservoirs. The Yitong (伊通) graben is situated in the northern section of the Tan-Lu (郯-庐) fault system in eastern China. It was characterized by dual properties of strike-slip and extension in Cenozoic. Two types of intrabasinal structures were identified as oblique fault and transverse uplift in the graben. The oblique faults arranged en echelon in plain and locally presented negative rosette structures on seismic profile, so they were closely derived from strike-slip movement of the northwestern boundary faults. Moreover, these oblique faults were divided to five zones. The three transverse uplifts, located corresponding to flattened southeast boundary faults, were mainly originated by displacement-gradient folding due to segmental extensional activities of southeast boundary faults. The large-scale sandbodies of subaqueous fan facies and fan delta facies had developed at the two types of intrabasinal structure zone. Based on analyzing the seismic facies, logging facies and seismic attribute extractions, and on discovering many incised valleys at the oblique fault zones, the two types of intrabasinal structures were revealed to have conducted drainage entering basin and further dispersing, and to have consequently controlled the development and distribution of sandbodies.

     

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