Origins of overpressure in the central Xihu depression of the East China Sea shelf basin

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Jingzhou Zhao ◽  
Zhiqiang Hou ◽  
Shuping Zhang ◽  
Mengna Chen
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pp. 1079-1093 ◽  
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Thomas S. Bianchi ◽  
Mead A. Allison ◽  
Piers Chapman ◽  
Guipeng Yang

2013 ◽  
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pp. 2244-2248 ◽  
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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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Pil-Hun Chang

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