Turbidite Fan Deposits in Gentle Slope Zones of Continental Faulted Basins: A Case Study from the Chezhen Depression, Bohai Bay Basin

Author:

Cheng Junyang1,He Xianke1,Duan Dongping1,Li Jingzhe23

Affiliation:

1. Shanghai Branch of CNOOC Ltd., Shanghai 200335, China

2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China

3. College of Electromechanics, Qingdao University of Science and Technology, Qingdao 266061, China

Abstract

Turbidite fans, serving as good reservoirs for petroleum accumulation, are typically formed during deep faulting periods in continental basins, particularly in steep slope zones. However, gentle slope zones are also significant and unique for the formation of turbidite fans. These turbidite fans hold immense importance in exploring concealed lithological reservoirs. Taking the Chezhen Depression of Bohai Bay Basin as an example, we conducted a comprehensive study of the turbidite fan deposits in the gentle slope zone. Our results indicate that (1) small-scale distal-source turbidite fans are a common sedimentary type in the Chezhen Depression of the Bohai Bay Basin; (2) the study area is mainly characterized by seven lithofacies; (3) there are incomplete Bouma sequences in the study interval. This study is an important turbidite investigation into continental faulted basins, and it can also provide an important reference value for exploration and development in unconventional reservoirs of the same type.

Funder

National Natural Science Foundation of China

Seven-Year Oil and Gas Action Plan of CNOOC

Chengdu University of Technology

Publisher

MDPI AG

Subject

Process Chemistry and Technology,Chemical Engineering (miscellaneous),Bioengineering

Reference45 articles.

1. Bouma, A.H. (1962). Sedimentology of Some Flysch Deposits: A Graphic Approach to Facies Interpretation, Elsevier.

2. Turbidites;Bouma;Developments in Sedimentology,1964

3. Key controls on the characteristics of turbidite systems;Bouma;Geol. Soc. Lond. Spec. Publ.,2004

4. The origin and significance of the internal sedimentary structures of turbidites;Walker;Proc. Yorks. Geol. Soc.,1965

5. Walker, R.G., and James, N.P. (1992). Facies Models: Response to Sea Level Change, GEO Text 1, Geological Association of Canada.

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