Vertical distribution of isoprenoid GDGTs in suspended particles from the East China Sea shelf and implications for sedimentary TEX86H records

2019 ◽  
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Da-Wei Li ◽  
Julian P. Sachs ◽  
Jingwen Hu ◽  
Yali Cao ◽  
...  
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Taku Wagawa ◽  
Toru Hasegawa ◽  
Kou Nishiuchi ◽  
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2020 ◽  
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Anchun Li ◽  
Xiting Liu ◽  
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2020 ◽  
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Xiaoshuang Li ◽  
Richard G. J. Bellerby ◽  
Philip Wallhead ◽  
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Jie Liu ◽  
...  

2018 ◽  
Vol 128 ◽  
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Lijun Zhao ◽  
Dantong Liu ◽  
Jinlong Wang ◽  
Jinzhou Du ◽  
Xiaolin Hou ◽  
...  

2013 ◽  
Vol 118 (3) ◽  
pp. 1079-1093 ◽  
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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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