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对东海扬子浅滩成因的再认识

刘振夏

刘振夏. 对东海扬子浅滩成因的再认识[J]. 海洋学报, 1996, 18(2): 85-92.
引用本文: 刘振夏. 对东海扬子浅滩成因的再认识[J]. 海洋学报, 1996, 18(2): 85-92.

对东海扬子浅滩成因的再认识

基金项目: 国家自然科学基金资助项目(编号:48970272).
  • 摘要: 本文依据前人资料,综合分析了位于东海西北部长江口东侧扬子浅滩的潮流作用、微地貌形态、物质成分和来源以及全新世沉积厚度,认为它是典型的现代潮流沙席,而不是古长江水下三角洲或陆架残留沉积.扬子浅滩潮流沙席与其西北部的江苏滨外潮流沙脊共同组成了长江口外现代潮流沉积体系.它们同属于太平洋潮波系统作用的潮流沉积环境.
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