SHALLOW SEISMIC RECORDS AND LATE PLEISTOCENE STRATIGRAPHY OF THE NORTH YELLOW SEA

CHEN Xiaohui; LI Rihui; XU Xiaoda

doi:10.3724/SP.J.1140.2011.03017

Marine Geology & Quaternary Geology > 2011 > 31(3): 17-22. > DOI: 10.3724/SP.J.1140.2011.03017

CHEN Xiaohui, LI Rihui, XU Xiaoda. SHALLOW SEISMIC RECORDS AND LATE PLEISTOCENE STRATIGRAPHY OF THE NORTH YELLOW SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(3): 17-22. DOI: 10.3724/SP.J.1140.2011.03017

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SHALLOW SEISMIC RECORDS AND LATE PLEISTOCENE STRATIGRAPHY OF THE NORTH YELLOW SEA

1 Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;
2 Key Laboratory of Marine Hydrocarbon Resource and Environmental Geology, MLR, Qingdao Institute of Marine Geology, Qingdao 266071;
3 Graduate School, Chinese Academy of Sciences, Beijing 100049, China

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Received Date: June 26, 2010
Revised Date: August 25, 2010

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Abstract

Abstract

High resolution shallow seismic profiles were interpreted in this paper for establishing the stratigraphic sequence of the North Yellow Sea. Nine stratigraphic units or sub-units (SU₁¹, SU₁², SU₁³, SU₂, SU₃, SU₄¹, SU₄², SU₄³, SU₅) were recognized based on the seismic data and some cores collected from this region. Results suggest that the stratigraphic units established upon shallow seismics are correlative with the core records obtained from previous studies. There occur three "transgression-regression" cycles. The stratigraphic units of SU₁,SU₃, SU₅ were respectively corresponding to the transgressive deposits formed in the marine isotope stage 1, marine isotope stage 3, and marine isotope stage 5, while the stratigraphic units of SU₂,SU₄ corresponding to the regressive deposits formed during the marine isotope stage 2 and marine isotope stage 4.
- shallow seismic profiles,
- the shallow seismic stratigraphy,
- the north Yellow Sea

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References

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SHALLOW SEISMIC RECORDS AND LATE PLEISTOCENE STRATIGRAPHY OF THE NORTH YELLOW SEA