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Volume 20 Issue 6
Dec 2009
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Article Contents
Chuanyan Huang, Hua Wang, Dunqing Xiao, Si Chen, Jiahao Wang, Yuantao Liao. Syndepositional fault controlling on depositional filling of the third member of Shahejie Formation in Beitang sag. Journal of Earth Science, 2009, 20(6): 949-958. doi: 10.1007/s12583-009-0080-6
Citation: Chuanyan Huang, Hua Wang, Dunqing Xiao, Si Chen, Jiahao Wang, Yuantao Liao. Syndepositional fault controlling on depositional filling of the third member of Shahejie Formation in Beitang sag. Journal of Earth Science, 2009, 20(6): 949-958. doi: 10.1007/s12583-009-0080-6

Syndepositional fault controlling on depositional filling of the third member of Shahejie Formation in Beitang sag

doi: 10.1007/s12583-009-0080-6
Funds:

the Research Institute of Exploration and Development, PetroChina Dagang Oilfield Company 

the National Natural Science Foundation of China 40872077

the Open Research Program of State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences GPMR200913

the Foundation of Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences TPR-2009-19

More Information
  • Corresponding author: Huang Chuanyan, cyhuang76@163.com
  • Received Date: 25 Dec 2008
  • Accepted Date: 30 Jul 2009
  • In the continental lake basin whose structures were extraordinarily active, tectonism is an important factor in controlling the sequence and the depositional filling of the basin. This article reports the assemble patterns of syndepositional fault in the third member of Shahejie (沙河街) Formation in Beitang (北塘) sag. The results show that the comb-shape fracture system and the fracture transformation zone were developed in Beitang sag. These assemble patterns obviously controlled the sand-body and spatial distribution of sedimentary system. However, the steep slope belt of fault terrace, the multistage slope belt and the low uplift gentle slope belt controlled the development of sequence styles. Analyses of the spatial-temporal relationship of the assemble pattern of syndepositional faults and the sedimentary system help predict the favorable exploration zone.

     

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