Astronomical forcing of the Paleogene coal-bearing hydrocarbon source rocks of the East China Sea Shelf Basin

2020 ◽  
Vol 406 ◽  
pp. 105715 ◽  
Author(s):  
Jingyu Zhang ◽  
Damien Pas ◽  
Wout Krijgsman ◽  
Wei Wei ◽  
Xuebin Du ◽  
...  
2012 ◽  
Vol 50-51 ◽  
pp. 41-53 ◽  
Author(s):  
Yutaka Yoshikawa ◽  
Takeshi Matsuno ◽  
Taku Wagawa ◽  
Toru Hasegawa ◽  
Kou Nishiuchi ◽  
...  

2020 ◽  
Vol 125 (10) ◽  
Author(s):  
Jiang Dong ◽  
Anchun Li ◽  
Xiting Liu ◽  
Shiming Wan ◽  
Fangjian Xu ◽  
...  

2020 ◽  
Vol 7 ◽  
Author(s):  
Xiaoshuang Li ◽  
Richard G. J. Bellerby ◽  
Philip Wallhead ◽  
Jianzhong Ge ◽  
Jie Liu ◽  
...  

2013 ◽  
Vol 118 (3) ◽  
pp. 1079-1093 ◽  
Author(s):  
Xinxin Li ◽  
Thomas S. Bianchi ◽  
Mead A. Allison ◽  
Piers Chapman ◽  
Guipeng Yang

2013 ◽  
Vol 807-809 ◽  
pp. 2244-2248 ◽  
Author(s):  
Jin Shui Liu ◽  
Ming Zhang ◽  
Jin Liang Zhang ◽  
Chun Yan Wang ◽  
Peng Hui Zhang

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.


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