Tectonic Evolution of the East China Sea Basin--Implication for the Development of the Western Pacific Marginal Seas: ABSTRACT

AAPG Bulletin ◽  
1994 ◽  
Vol 78 ◽  
Author(s):  
G. Ming Wang, Michael P. Coward, We
Keyword(s):  
East China Sea ◽  
Tectonic Evolution ◽  
Western Pacific ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Marginal Seas ◽  
The Western Pacific ◽  
East China Sea Basin

scholarly journals Tectonic Evolution Review of the East China Sea Basin

2019 ◽  
Author(s):  
Bing Wang
Keyword(s):  
East China Sea ◽  
Tectonic Evolution ◽  
Leading Edge ◽  
East China ◽  
Eurasian Plate ◽  
The East China Sea ◽  
China Sea ◽  
East China Sea Shelf ◽  
Back Arc ◽  
East China Sea Basin

The back-arc East China Sea Basin lies on extended continental crust at the leading edge of the Eurasian plate. Geology over the East China Sea Shelf Basin have been studied bits and pieces by various researchers over the past 20 years. This work is intended to provide a full review of the tectonic evolution over the East China Sea Basin. 

Tectonic Evolution and Sequence Filling of Paleocene in Lishui Sag, East China Sea Shelf Basin

2013 ◽  
Vol 807-809 ◽  
pp. 2244-2248 ◽  
Author(s):  
Jin Shui Liu ◽  
Ming Zhang ◽  
Jin Liang Zhang ◽  
Chun Yan Wang ◽  
Peng Hui Zhang
Keyword(s):  
East China Sea ◽  
Tectonic Evolution ◽  
Sedimentary Facies ◽  
East China ◽  
The East China Sea ◽  
Control Effect ◽  
Third Order ◽  
China Sea ◽  
East China Sea Shelf ◽  
System Tracts

The Lishui sag located at Southwest of the East China Sea Shelf Basin. It had undergone the four stages of syn-rift processes in Late Cretaceous to Paleocene: initial rift stage, main rift stage, stable rift stage and decline stage. The tectonic evolution has control effect on the development of sequence stratigraphy and the sediments distribution. Three second-order sequences, five third-order sequences and twelve system tracts are distinguished. Different sedimentary facies recognized in the Lishui sag.

Fold growth during basin inversion — example from the East China Sea Basin

1995 ◽  
Vol 88 (1) ◽  
pp. 493-522 ◽  
Author(s):  
Guang Ming Wang ◽  
Mike P. Coward ◽  
Wenguang Yuan ◽  
Shenshu Liu ◽  
Wenqiang Wang
Keyword(s):  
East China Sea ◽  
East China ◽  
The East China Sea ◽  
Basin Inversion ◽  
China Sea ◽  
East China Sea Basin

Discussion of seismic diagenetic facies of deep reservoir in the East China Sea Basin

2021 ◽  
pp. 109352
Author(s):  
Wenguang Wang ◽  
Chengyan Lin ◽  
Xianguo Zhang ◽  
Chunmei Dong ◽  
Lihua Ren ◽  
...  
Keyword(s):  
East China Sea ◽  
East China ◽  
The East China Sea ◽  
China Sea ◽  
Deep Reservoir ◽  
Diagenetic Facies ◽  
East China Sea Basin

Classification and origin of natural gases from Lishui Sag, the East China Sea Basin

2008 ◽  
Vol 51 (S1) ◽  
pp. 122-130 ◽  
Author(s):  
JianPing Chen ◽  
HePing Ge ◽  
XiaoDong Chen ◽  
ChunPing Deng ◽  
DiGang Liang
Keyword(s):  
East China Sea ◽  
East China ◽  
The East China Sea ◽  
Natural Gases ◽  
China Sea ◽  
East China Sea Basin

Interannual variability of typhoon-induced northeast Asian marginal seas-mean sea level

2021 ◽  
Author(s):  
MyeongHee Han ◽  
SungHyun Nam
Keyword(s):  
Sea Level ◽  
East China Sea ◽  
East China ◽  
Interannual Variations ◽  
The East China Sea ◽  
Mean Sea Level ◽  
China Sea ◽  
Marginal Seas ◽  
Pass Through ◽  
Northeast Asian

<p><span>As connected through relatively narrow and shallow straits, inflow and outflow volume transports of the northeast Asian marginal seas (NEAMS) are strongly forced to yield significant convergence or divergence and resulting rise or drop in spatially-averaged sea level. Here, we examined interannual variations of August NEAMS-mean sea level observed from satellite altimetry from 1993 to 2019. Typhoon activity was found to be a primary factor controlling the interannual variations of NEAMS-mean sea level in August. Relatively high August sea level over the NEAMS is derived in years when more typhoons pass through the East China Sea (Period H) due to typhoon-induced Ekman transports. The resultant NEAMS-mean sea level is a few cm higher than that during the years of less or no typhoon activity in the East China Sea (Period L). This study highlights the importance of typhoon (hurricane) activity on interannual variations of regional sea level in the mid-latitude and semi-enclosed marginal seas.</span></p>

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