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Sheng Haojie. Subbottom Profiling and Its Geological Interpretation on the Southern Margin of Continental Shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 1999, 17(1): 78-83.
Citation: Sheng Haojie. Subbottom Profiling and Its Geological Interpretation on the Southern Margin of Continental Shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 1999, 17(1): 78-83.

Subbottom Profiling and Its Geological Interpretation on the Southern Margin of Continental Shelf of the East China Sea

  • Received Date: 1998-04-21
  • Rev Recd Date: 1998-10-06
  • Publish Date: 1999-03-10
  • It is expounded the probing of the high resolution subbottom profile on the southern margin of the continental Shelf of the East China Sea.According to the data of subbottom profile the detail geological interpretations are as follows:①the high resolution subbottom profiles record the submarine topography,geomorphy and sedimentary structures of the study area directly,which can be used for studing the sedimentary environment and geolgical history;②three paleao-river valleys have been probed and it is shown that the shoreline of china Sea shelf in the umu galacial(Late Pleistocene Epoch) maybe was 150 m below the present sea levef;③ in this area,the complicated geomorophy and structures is related to the earthguake、volcanicity,and soon.
  • [1] 1 潘国富.浅岐地震声学剖面的声地层学解释.海洋地质与第四纪地质.1991,11(1):93~104

    2 秦蕴珊.东海地质,北京:科学出版社,1987.

    3 金翔龙.东海海洋地质.北京:海洋出版社,1992.67~77

    4 沈华梯.东海陆架残留沉积时代和成因模式.海洋学报,1987
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  • Received:  1998-04-21
  • Revised:  1998-10-06
  • Published:  1999-03-10

Subbottom Profiling and Its Geological Interpretation on the Southern Margin of Continental Shelf of the East China Sea

Abstract: It is expounded the probing of the high resolution subbottom profile on the southern margin of the continental Shelf of the East China Sea.According to the data of subbottom profile the detail geological interpretations are as follows:①the high resolution subbottom profiles record the submarine topography,geomorphy and sedimentary structures of the study area directly,which can be used for studing the sedimentary environment and geolgical history;②three paleao-river valleys have been probed and it is shown that the shoreline of china Sea shelf in the umu galacial(Late Pleistocene Epoch) maybe was 150 m below the present sea levef;③ in this area,the complicated geomorophy and structures is related to the earthguake、volcanicity,and soon.

Sheng Haojie. Subbottom Profiling and Its Geological Interpretation on the Southern Margin of Continental Shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 1999, 17(1): 78-83.
Citation: Sheng Haojie. Subbottom Profiling and Its Geological Interpretation on the Southern Margin of Continental Shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 1999, 17(1): 78-83.
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