珠江口外海域滨海断裂带沿构造走向的变化特征

熊成; 曹敬贺; 孙金龙; 夏少红; 万奎元; 范朝焰; 杨碧峰

doi:10.3799/dqkx.2018.553

Volume 43 Issue 10

Oct. 2018

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Article Navigation > Earth Science > 2018 > 43(10): 3682-3697

Xiong Cheng, Cao Jinghe, Sun Jinlong, Xia Shaohong, Wan Kuiyuan, Fan Chaoyan, Yang Bifeng, 2018. Variation Characteristics along the Strike of the Littoral Fault Zone in Offshore Pearl River Estuary. Earth Science, 43(10): 3682-3697. doi: 10.3799/dqkx.2018.553

Citation:

Xiong Cheng, Cao Jinghe, Sun Jinlong, Xia Shaohong, Wan Kuiyuan, Fan Chaoyan, Yang Bifeng, 2018. Variation Characteristics along the Strike of the Littoral Fault Zone in Offshore Pearl River Estuary. Earth Science, 43(10): 3682-3697. doi: 10.3799/dqkx.2018.553

Citation:

Xiong Cheng, Cao Jinghe, Sun Jinlong, Xia Shaohong, Wan Kuiyuan, Fan Chaoyan, Yang Bifeng, 2018. Variation Characteristics along the Strike of the Littoral Fault Zone in Offshore Pearl River Estuary. Earth Science, 43(10): 3682-3697. doi: 10.3799/dqkx.2018.553

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Variation Characteristics along the Strike of the Littoral Fault Zone in Offshore Pearl River Estuary

doi: 10.3799/dqkx.2018.553

1.
CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China
2.
University of Chinese Academy of Science, Beijing 100049, China

Received Date: 2017-11-15
Publish Date: 2018-10-20

Abstract

Abstract

The Littoral Fault Zone (LFZ) is an important seismic control and seismic structure in the northern continental margin of the South China Sea.The study of LFZ is related to regional seismic resistance, crustal stability evaluation and the understanding of tectonic evolution of the South China Sea. To find out the spatial variations along the strike of the LFZ, we processed the data of the onshore-offshore deep seismic experiment in Pearl River Estuary (PRE) area in 2015 and simulated a P-wave velocity model in the western PRE and detected the general location of LFZ. The results show that the LFZ dips southeast down to the Moho with a low velocity of 5.3-6.7 km/s in the crust. The basement fluctuates greatly and the depth of the Moho interface is decreases gradually from 28.5 km to 24.5 km from the onshore to offshore. Compared with previous studies in the eastern PRE, the general morphological characteristics of the LFZ on both sides of the PRE are similar. However they also show obvious differences. From east to west, the structure of the fault zone becomes more complex, with steped normal faults developed and the northern boundary fault moves northward a distance and changes into low angle normal fault with small fracture distance from steep normal fault with large break distance, and the low velocity anomaly in the fault zone gradually decreases. The results not only deepen the understanding of the shallow and deep structure of LFZ, but also provide a reference for the seismotectonics of the northern continental margin of South China Sea.
- the Pearl River Estuary,
- the littoral fault zone,
- crustal structure,
- deep seismic experiment,
- geophysics

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References(117)

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Variation Characteristics along the Strike of the Littoral Fault Zone in Offshore Pearl River Estuary

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