东海西南陆架表层沉积物粒度分布特征

田姗姗, 张富元, 阎丽妮, 徐轩. 东海西南陆架表层沉积物粒度分布特征[J]. 海洋地质与第四纪地质, 2009, 29(5): 13-20. doi: 10.3724/SP.J.1140.2009.05013
引用本文: 田姗姗, 张富元, 阎丽妮, 徐轩. 东海西南陆架表层沉积物粒度分布特征[J]. 海洋地质与第四纪地质, 2009, 29(5): 13-20. doi: 10.3724/SP.J.1140.2009.05013
TIAN Shanshan, ZHANG Fuyuan, YAN Lini, XU Xuan. DISTRIBUTION CHARACTERISTICS OF GRANULARITIES OF SURFACE SEDIMENTS IN THE SOUTHWESTERN SHELF OF THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 13-20. doi: 10.3724/SP.J.1140.2009.05013
Citation: TIAN Shanshan, ZHANG Fuyuan, YAN Lini, XU Xuan. DISTRIBUTION CHARACTERISTICS OF GRANULARITIES OF SURFACE SEDIMENTS IN THE SOUTHWESTERN SHELF OF THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 13-20. doi: 10.3724/SP.J.1140.2009.05013

东海西南陆架表层沉积物粒度分布特征

  • 基金项目:

    国家海洋局海底科学重点实验室开放基金项目"中国东部沿海第四纪阶地沉积释光测年研究"

详细信息
    作者简介: 田姗姗(1984-),女,硕士,主要从事海洋沉积和地震沉积学研究,E-mail:tianshansh-15@163.com
  • 中图分类号: P736.21

DISTRIBUTION CHARACTERISTICS OF GRANULARITIES OF SURFACE SEDIMENTS IN THE SOUTHWESTERN SHELF OF THE EAST CHINA SEA

  • 利用东海西南陆架65个表层沉积物样品的粒度分析资料,进行了粒度参数的计算与Q型聚类分析,进而探讨研究区表层沉积物的粒度分布特征。研究区表层沉积物的主要粒级是4~10 Φ(粗粉砂-粗黏土),由岸向海粒度变粗;沉积物总体上分选差,但由岸向海分选变好。Q型聚类分析表明,研究区的沉积物分为内陆架细粒沉积物和外陆架粗粒沉积物两类,平行于海岸线分布,123°E左右是两类沉积物的分界线。对比不同站位的沉积物粒度累积曲线,判断两类沉积物属于不同的成因类型,内陆架的细粒沉积物是现代近岸沉积,外陆架的粗粒沉积物与现今的沉积环境不符,属于残留沉积。
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收稿日期:  2009-03-24
修回日期:  2009-08-01

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