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东海外陆架晚第四纪若干沉积学问题的研究现状与展望

王中波 杨守业 张志珣 李日辉 蓝先洪 印萍 张训华

王中波, 杨守业, 张志珣, 李日辉, 蓝先洪, 印萍, 张训华. 东海外陆架晚第四纪若干沉积学问题的研究现状与展望[J]. 海洋地质与第四纪地质, 2012, 32(3): 1-10. doi: 10.3724/SP.J.1140.2012.03001
引用本文: 王中波, 杨守业, 张志珣, 李日辉, 蓝先洪, 印萍, 张训华. 东海外陆架晚第四纪若干沉积学问题的研究现状与展望[J]. 海洋地质与第四纪地质, 2012, 32(3): 1-10. doi: 10.3724/SP.J.1140.2012.03001
WANG Zhongbo, YANG Shouye, ZHANG Zhixun, LI Rihui, LAN Xianhong, YIN Ping, ZHANG Xunhua. A REVIEW OF THE LATE QUATERNARY SEDIMENTOLOGICAL STUDIES ON THE OUTER SHELF OF THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2012, 32(3): 1-10. doi: 10.3724/SP.J.1140.2012.03001
Citation: WANG Zhongbo, YANG Shouye, ZHANG Zhixun, LI Rihui, LAN Xianhong, YIN Ping, ZHANG Xunhua. A REVIEW OF THE LATE QUATERNARY SEDIMENTOLOGICAL STUDIES ON THE OUTER SHELF OF THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2012, 32(3): 1-10. doi: 10.3724/SP.J.1140.2012.03001

东海外陆架晚第四纪若干沉积学问题的研究现状与展望


doi: 10.3724/SP.J.1140.2012.03001
详细信息
    作者简介:

    王中波(1979-),男,博士生,助理研究员,主要从事海洋沉积研究,E-mail:my_zhongbo@163.com

  • 基金项目:

    "大陆架科学钻探"项目(GZH201100202)

    中国地质调查局海洋地质调查工作项目(GHZ201100203)

    中国地质调查局国土资源大调查项目(GZH200800501,1212010611301)

    国家自然科学基金项目(41040041)

    国土资源部海洋油气资源与环境地质重点实验室开放基金(MRE200917)

  • 中图分类号: P736.2

A REVIEW OF THE LATE QUATERNARY SEDIMENTOLOGICAL STUDIES ON THE OUTER SHELF OF THE EAST CHINA SEA

More Information
  • 摘要: 我国东海陆架尤其外陆架的晚第四纪沉积地层、古河道沉积与下切河谷充填沉积、潮流沙脊沉积研究等已经取得较多研究成果,综述已有的研究认识和关键科学问题,讨论地层研究中的氧同位素2期和4期地层划分出现的争议、不同的地层演化模式以及与之紧密相关的末次冰盛期古河道的存在与演化、东海陆架冰后期潮流沙脊成因研究中存在的不同观点,提出未来东海外陆架晚第四纪沉积学研究的思路和工作展望。
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出版历程
  • 收稿日期:  2011-11-04
  • 修回日期:  2012-03-18

东海外陆架晚第四纪若干沉积学问题的研究现状与展望

doi: 10.3724/SP.J.1140.2012.03001
    作者简介:

    王中波(1979-),男,博士生,助理研究员,主要从事海洋沉积研究,E-mail:my_zhongbo@163.com

基金项目:

"大陆架科学钻探"项目(GZH201100202)

中国地质调查局海洋地质调查工作项目(GHZ201100203)

中国地质调查局国土资源大调查项目(GZH200800501,1212010611301)

国家自然科学基金项目(41040041)

国土资源部海洋油气资源与环境地质重点实验室开放基金(MRE200917)

  • 中图分类号: P736.2

摘要: 我国东海陆架尤其外陆架的晚第四纪沉积地层、古河道沉积与下切河谷充填沉积、潮流沙脊沉积研究等已经取得较多研究成果,综述已有的研究认识和关键科学问题,讨论地层研究中的氧同位素2期和4期地层划分出现的争议、不同的地层演化模式以及与之紧密相关的末次冰盛期古河道的存在与演化、东海陆架冰后期潮流沙脊成因研究中存在的不同观点,提出未来东海外陆架晚第四纪沉积学研究的思路和工作展望。

English Abstract

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