Tectonic framework research in Zhujiang River Mouth Basin based on gravity and magnetic data

He Zeyang; Bai Zhizhao; Wang Wanyin; Li Linzhi; Zhang Yimi; Chen Ying; He Tao; Ma Ruiyun

doi:10.12284/hyxb2023165

Volume 45 Issue 12

Dec. 2023

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He Zeyang，Bai Zhizhao，Wang Wanyin, et al. Tectonic framework research in Zhujiang River Mouth Basin based on gravity and magnetic data[J]. Haiyang Xuebao，2023, 45(12)：25–43 doi: 10.12284/hyxb2023165

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Tectonic framework research in Zhujiang River Mouth Basin based on gravity and magnetic data

doi: 10.12284/hyxb2023165

He Zeyang^1
,,
Bai Zhizhao²,
Wang Wanyin^{1, 3, 4
,
,},
Li Linzhi²,
Zhang Yimi^{1, 5},
Chen Ying²,
He Tao^{1, 5},
Ma Ruiyun¹

1.
School of Geology Engineering and Geomatics, Chang’an University, Xi’an 710054, China
2.
CNOOC Research Institude Co., Ltd., Beijing 100028, China
3.
National Engineering Research Center of Offshore Oil and Gas Exploration, Beijing 100028, China
4.
Key Laboratory of Marine Geology and Environment, Chinese Academy of Science, Qingdao 266071, China
5.
Department of Earth Sciences, Memorial University of Newfoundland, St. Johns AlB3X5, Canada

Received Date: 2023-05-04
Rev Recd Date: 2023-09-28

Available Online: 2024-01-09

Publish Date: 2023-12-01

Abstract

Abstract

The Zhujiang River Mouth Basin is located in the northern shelf of the South China Sea, and its tectonic evolution is very complicated. At the same time, as one of the hydrocarbon-rich basins in offshore China, Zhujiang River Mouth Basin ranks the top in oil and gas production among the offshore basins. With the deepening of exploration, the boundary of the Zhujiang River Mouth Basin has been changing, and the southern boundary of the basin is disputed. In this paper, based on satellite gravity and magnetic anomaly data, the fault distribution of Zhujiang River Mouth Basin is re-studied and the plane location of igneous rocks is identified. The Cenozoic thickness of the study area is retrieved with high-precision seismic data, and the tectonic units of the study area are adjusted according to the processing results. The results show that the fault distribution in the study area is mainly NEE, NE and NW trending. In this study, four new faults were identified based on the satellite gravity data. The overall strike of the igneous rocks in the plane is NEE strike, but there are differences among different regional strikes. There are nearly EW trending igneous rocks in the western basin, NWW trending igneous rocks in the central basin, and no other strike in the eastern basin. According to gravity data and Cenozoic characteristics, Yangjiang Sag is divided into Yangjiang West Sag and Yangjiang East Sag, and Wenchang D Sag and Wenchang E Sag are deleted. The Beiweitan Fault is the same as the Yangjiang-Yitong Fault, which divides the basin into three parts: the west, the middle and the east. The fault strike, the plane position of igneous rock, the thickness of Cenozoic and the tectonic units of the three parts are different. The study of faults, igneous rocks and tectonic units in Zhujiang River Mouth Basin aims to provide geophysical support for subsequent basin research and oil and gas breakthrough.
- gravity and magnetic data,
- faults,
- igneous rocks,
- Cenozoic surface

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