Crustal structure of the Gunsan Basin in the SE Yellow Sea from ocean bottom seismometer (OBS) data and its linkage to the South China Block

2019 ◽  
Vol 180 ◽  
pp. 103881 ◽  
Author(s):  
Han-Joon Kim ◽  
Chung-Ho Kim ◽  
Tianyao Hao ◽  
Lihua Liu ◽  
Kwang-Hee Kim ◽  
...  
Keyword(s):  
South China ◽  
Crustal Structure ◽  
Yellow Sea ◽  
Ocean Bottom ◽  
Ocean Bottom Seismometer ◽  
South China Block ◽  
The South ◽  
Obs Data

A Wide Angle Ocean Bottom Seismometer Experiment Across Liyue Bank, the Southern Margin of the South China Sea

2011 ◽  
Vol 54 (6) ◽  
pp. 1033-1044 ◽  
Author(s):  
Ai-Guo RUAN ◽  
Xiong-Wei NIU ◽  
Xue-Lin QIU ◽  
Jia-Biao LI ◽  
Zhen-Li WU ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
Ocean Bottom ◽  
Ocean Bottom Seismometer ◽  
Wide Angle ◽  
The South ◽  
China Sea ◽  
Southern Margin

Spatio-temporal evolution and dynamic origin of Jurassic-Cretaceous magmatism in the South China Block

2021 ◽  
Vol 217 ◽  
pp. 103605
Author(s):  
Xianzhi Cao ◽  
Nicolas Flament ◽  
Sanzhong Li ◽  
R. Dietmar Müller
Keyword(s):  
South China ◽  
Temporal Evolution ◽  
South China Block ◽  
The South ◽  
Spatio Temporal ◽  
Cretaceous Magmatism

Typhoon-Induced Microseisms around the South China Sea

2020 ◽  
Vol 91 (6) ◽  
pp. 3454-3468
Author(s):  
Seongjun Park ◽  
Tae-Kyung Hong
Keyword(s):  
South China Sea ◽  
South China ◽  
Bottom Topography ◽  
Pressure Change ◽  
Ocean Waves ◽  
The South China Sea ◽  
Ocean Bottom ◽  
The South ◽  
China Sea ◽  
Regional Factors

Abstract Microseisms in frequencies of 0.05–0.5 Hz are a presentation of solid earth response to the ocean waves that are developed by atmospheric pressure change. The South China Sea provides a natural laboratory with a closed ocean environment to examine the influence of regional factors on microseism development as well as the nature of microseisms. The microseisms induced by typhoons crossing over the South China Sea are investigated. Typhoons are typical transient sources of varying strengths and locations. Primary microseisms develop nearly stationary in the northeastern South China Sea for most typhoons, suggesting effective environment for excitation of primary microseisms. Typhoon-induced secondary microseisms develop around the typhoon paths with time delays varying up to one day. Typhoon-induced microseism amplitudes are proportional to the ocean-wave amplitudes in the source regions, decaying with distance. Ocean waves develop following the typhoons for days. The dominant frequency of typhoon-induced microseisms increases with time due to the influence of dispersive ocean waves. The microseisms are affected by regional factors including crustal structures, coastal geometry, ocean depth, and ocean-bottom topography.

scholarly journals Crustal structure and extension mode in the northwestern margin of the South China Sea

2016 ◽  
Vol 17 (6) ◽  
pp. 2143-2167 ◽  
Author(s):  
Jinwei Gao ◽  
Shiguo Wu ◽  
Kirk McIntosh ◽  
Lijun Mi ◽  
Zheng Liu ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
Crustal Structure ◽  
The South China Sea ◽  
The South ◽  
China Sea ◽  
Northwestern Margin

scholarly journals Thrusting, exhumation and basin fill on the western margin of the South China block during India-Asian collision

2018 ◽  
Author(s):  
Kai Cao ◽  
Guocan Wang ◽  
Philippe Hervé Leloup ◽  
Wei Mahéo ◽  
Yadong Xu ◽  
...  
Keyword(s):  
South China ◽  
South China Block ◽  
The South ◽  
Western Margin ◽  
Basin Fill
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