Gravity anomaly and fine crustal structure in the middle segment of the Tan-Lu fault zone, eastern Chinese mainland

2021 ◽  
pp. 105027
Author(s):  
Xin Wang ◽  
Wenliang Jiang ◽  
Jingfa Zhang ◽  
Wenhao Shen ◽  
Zhihao Fu
Keyword(s):  
Gravity Anomaly ◽  
Fault Zone ◽  
Crustal Structure ◽  
Chinese Mainland ◽  
Middle Segment

An Analysis on Deep Crustal Structure Along the Onshore-Offshore Seismic Profile Across the Binghai (Littoral) Fault Zone in Ne South China Sea

2004 ◽  
Vol 47 (5) ◽  
pp. 954-961 ◽  
Author(s):  
Ming-Hui ZHAO ◽  
Xue-Lin QIU ◽  
Chun-Ming YE ◽  
Kan-Yuan XIA ◽  
Ci-Liu HUANG ◽  
...  
Keyword(s):  
South China Sea ◽  
Fault Zone ◽  
South China ◽  
Crustal Structure ◽  
Seismic Profile ◽  
China Sea ◽  
Deep Crustal Structure

Holocene activity evidence on the southeast boundary fault of Heqing basin, middle segment of Heqing-Eryuan fault zone, West Yunnan Province, China

2017 ◽  
Vol 14 (7) ◽  
pp. 1445-1453 ◽  
Author(s):  
Chang-bin Sun ◽  
De-wen Li ◽  
Xiao-ming Shen ◽  
Yan-rui Kang ◽  
Rui Liu ◽  
...  
Keyword(s):  
Fault Zone ◽  
Yunnan Province ◽  
Middle Segment ◽  
Boundary Fault ◽  
Holocene Activity ◽  
Heqing Basin

Crustal Thickness of Chinese Mainland Inversed by GOCE Satellite Gravity Data

2014 ◽  
Vol 568-570 ◽  
pp. 288-291
Author(s):  
Hai Jun Xu ◽  
Hu Rong Duan ◽  
Jian Ye Zhou
Keyword(s):  
Comparative Analysis ◽  
Gravity Anomaly ◽  
Gravity Data ◽  
Crustal Thickness ◽  
Geoid Height ◽  
Chinese Mainland ◽  
Satellite Gravity ◽  
Inversion Result ◽  
Goce Satellite

GOCE satellite gravity data is often used to compute gravity anomaly and geoid height. In the paper, GOCE gravity data is used to inverse the crustal thickness of Chinese mainland (E70°~130°, N20°~50°) in this paper. In order to test the reliability of the result, the computing result is compared with previous studies. The comparative analysis shows that the inversion result by GOCE gravity data has higher resolution and has good consistence with the previous studies.

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