NEOTECTONIC MOVEMENT IN THE EASTERN BOZHONG DEPRESSION

TONG Siyou; CHEN Renjie; LIU Huaishan; ZHAO Tiehu; YIN Yanxin

doi:10.16562/j.cnki.0256-1492.2015.06.007

2015 Vol. 35, No. 6

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TONG Siyou, CHEN Renjie, LIU Huaishan, ZHAO Tiehu, YIN Yanxin. NEOTECTONIC MOVEMENT IN THE EASTERN BOZHONG DEPRESSION[J]. Marine Geology & Quaternary Geology, 2015, 35(6): 73-79. doi: 10.16562/j.cnki.0256-1492.2015.06.007

Citation:

TONG Siyou, CHEN Renjie, LIU Huaishan, ZHAO Tiehu, YIN Yanxin. NEOTECTONIC MOVEMENT IN THE EASTERN BOZHONG DEPRESSION[J]. Marine Geology & Quaternary Geology, 2015, 35(6): 73-79. doi: 10.16562/j.cnki.0256-1492.2015.06.007

NEOTECTONIC MOVEMENT IN THE EASTERN BOZHONG DEPRESSION

1. Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Ocean University of China, Qingdao 266100, China;
2. Shenzhen Branch of CNOOC Ltd., Guangzhou 510240;
3. Qingdao Institute of Marine Geology, Qingdao 266071, China

Received Date: 20 April 2015

Revised Date: 09 November 2015

Abstract

Abstract

The eastern Bozhong Depression is one of the areas with most intense neotectonism in China. There are complex neotectonic structures and types and it is still the most important earthquake area in eastern China.The neotectonic characteristics in the deep part have been disclosed by petroleum exploration, but the features in the shallow part remain unknown due to limited shallow seismic surveys.Based on the 2000km of latest high-resolution multi-channel seismic data,this paper has made a detailed study of the neotectonism in geometry,kinematics,earthquake activities,sedimentation and depocenter migration.According to the deep and regional tectonic backgrounds,it is deduced that the neotectonic movement of the region is a kind of extensional movement resulted from the strike-slip faulting superimposed on the deeplevel thermal subsidence.
- neotectonism /
- high-resolution multi-channel seismic exploration /
- Quaternary /
- the Bozhong Depression

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References

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