HYDROCARBON ACCUMULATION IN ZENGMU PULL-APART BASIN:INSIGHTS FROM THE CONTROL OF TINJAR-WEST BARAM LINE

ZHAO Feiyu; JIANG Suhua; LI Sanzhong; MENG Fanshun; CAO Wei; WANG Gang; ZHANG Huixuan; GAO Song; ZHENG Qiliang

doi:10.16562/j.cnki.0256-1492.2017.04.014

Marine Geology & Quaternary Geology > 2017 > 37(4): 209-220. > DOI: 10.16562/j.cnki.0256-1492.2017.04.014

ZHAO Feiyu, JIANG Suhua, LI Sanzhong, MENG Fanshun, CAO Wei, WANG Gang, ZHANG Huixuan, GAO Song, ZHENG Qiliang. HYDROCARBON ACCUMULATION IN ZENGMU PULL-APART BASIN:INSIGHTS FROM THE CONTROL OF TINJAR-WEST BARAM LINE[J]. Marine Geology & Quaternary Geology, 2017, 37(4): 209-220. DOI: 10.16562/j.cnki.0256-1492.2017.04.014

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HYDROCARBON ACCUMULATION IN ZENGMU PULL-APART BASIN:INSIGHTS FROM THE CONTROL OF TINJAR-WEST BARAM LINE

ZHAO Feiyu^1,2,,
JIANG Suhua^1,2, ,,
LI Sanzhong^1,2,
MENG Fanshun^1,2,
CAO Wei^1,2,
WANG Gang^1,2,
ZHANG Huixuan^1,2,
GAO Song^1,2,
ZHENG Qiliang^1,2

1.
Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Qingdao 266100, China
2.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China

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Received Date: May 30, 2017
Revised Date: July 19, 2017

Graphical Abstract

Abstract

Abstract

The Tinjar-West Baram Line of the Southern South China Sea is a northwest-trending strike-slip fault. As the boundary between the Zengmu Basin and the Beikang Basin and Nansha Trough, the strike-slip fault of the Tinjar-West Baram Line was first activated in Oligocene as a intensely dextral strike-slip fault, then turned to sinistral after late Miocene and, then turned to dextral again since Pleistocene up to present. Based upon the study of seismic profiles, gravity and magnetic data, geothermal heat flux distribution data near the Tinjar-West Baram Line, we studied the crustal nature and lithosphere thickness of the Zengmu Basin, and discussed the control of Tinjar-West Baram Line over the evolution and accumulation of hydrocarbon in the Zengmu Basin. It is concluded that the faulting of the Tinjar-West Baram Line had provided rich source of sediments for the Zengmu Basin. The strike slipping of the faults helped the formation of the good traps in the Zengmu Basin, and the reversed strike slipping in the late period led to the northward motion of the basin depocenters. The faults are important channels to the deep heat source, beneficial to the hydrocarbon generation, and the secondary faults are also the major passages for hydrocarbon migration.
- Tinjar-West Baram Line,
- strike-slip fault,
- hydrocarbon accumulation,
- Zengmu Basin

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References (45)

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