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

Jin Shui Liu; Ming Zhang; Jin Liang Zhang; Chun Yan Wang; Peng Hui Zhang

doi:10.4028/www.scientific.net/AMR.807-809.2244

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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 807-809Tectonic Evolution and Sequence Filling of...

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

Abstract:

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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Periodical:

Advanced Materials Research (Volumes 807-809)

Pages:

2244-2248

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.807-809.2244

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Online since:

September 2013

Authors:

Jin Shui Liu, Ming Zhang, Jin Liang Zhang, Chun Yan Wang, Peng Hui Zhang

Keywords:

Lishui Sag, Paleocene, Sequence Filling, Stratigraphic Framework, Tectonic Evolution

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References

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