Sea-Level Rise and Sedimentary Environment Response in the <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on">East China</st1:place> Continental Shelf since the Last Glacial Maximum <?xml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p></o:p>

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line-level: 2" class=MsoNormal>Sea-Level Rise and Sedimentary Environment Response in the oft-com:office:smarttags" />East China Continental Shelf since the Last Glacial Maximum oft-com:office:office" />

详细信息

责任者：Li Guangxue (College of Marine Geosciences ; Ocean University of China ; Qingdao 266100 ; China) ; Liu Yong
刊名：Marine Geology & Quaternary Geology
出版年：2009
卷期：29(4)
关键词：全新世 ; Holocene ; 大陆架环境 ; shelf environment ; 海平面升降 ; eustacy ; 末次冰期 ; last glacial age ; 中国 ; China
页码：p.13-19
图表：3 illus., 35 refs.
分类号：1400
issnNo：ISSN0256-1492
isbnNo：CN37-1117/P

摘要

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Up to now, there is no study on large-scale continental shelf system response to global sea level change. In this paper, seafloor sediments in the oft-com:office:smarttags" />East China Sea broad continental shelf have been researched in detail by mapping in the past five years. The results show that there is a good response relationship between distribution of modern sedimentary environment in the East China shelf and sea level change since LGM. The seafloor is covered by three sedimentary systems in modern East China shelf, which are ancient onshore zone at the phase of low sea level, transgressive system during the Last Deglaciation and eddy and offshore sedimentary system in the period of high sea level.

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