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南海渐新世以来粘土矿物的演变特征及意义

唐松 邵磊 赵泉鸿

唐松, 邵磊, 赵泉鸿. 南海渐新世以来粘土矿物的演变特征及意义[J]. 沉积学报, 2004, 22(2): 337-342.
引用本文: 唐松, 邵磊, 赵泉鸿. 南海渐新世以来粘土矿物的演变特征及意义[J]. 沉积学报, 2004, 22(2): 337-342.
TANG Song, SHAO Lei, ZHAO Quan-hong. Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance[J]. Acta Sedimentologica Sinica, 2004, 22(2): 337-342.
Citation: TANG Song, SHAO Lei, ZHAO Quan-hong. Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance[J]. Acta Sedimentologica Sinica, 2004, 22(2): 337-342.

南海渐新世以来粘土矿物的演变特征及意义

基金项目: 国家自然科学基金项目(批准号:49999560,40276019);国家重点基础研究发展规划项目(G2000078500)资助
详细信息
    作者简介:

    唐松,男 1979年出生,硕士研究生,海洋地质学

  • 中图分类号: P736.21

Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance

  • 摘要: 通过对南海北部ODP184航次1148站32.8Ma以来深海沉积物中粘土矿物组成及其变化特征的分析,发现以15.5Ma为界,下部沉积物粘土矿物组成中蒙脱石含量高达70%,上部则以伊利石和绿泥石逐步增高、蒙脱石含量明显下降为特征,揭示出该区深海沉积物中粘土矿物演变可以分为32.8~15.5Ma的构造控制期和15.5Ma以来的气候控制期。在构造控制期,粘土矿物成分记录了南海扩张演变的历史;而在气候控制期,粘土矿物特征除反映出南海北部周边总体降温的过程外,还显示了3Ma的突然降温,与该站底栖有孔虫氧同位素资料反映的全球气候变化具有很好的对比性。
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出版历程
  • 收稿日期:  2003-05-28
  • 修回日期:  2003-11-24
  • 刊出日期:  2004-06-10

目录

    南海渐新世以来粘土矿物的演变特征及意义

      基金项目:  国家自然科学基金项目(批准号:49999560,40276019);国家重点基础研究发展规划项目(G2000078500)资助
      作者简介:

      唐松,男 1979年出生,硕士研究生,海洋地质学

    • 中图分类号: P736.21

    摘要: 通过对南海北部ODP184航次1148站32.8Ma以来深海沉积物中粘土矿物组成及其变化特征的分析,发现以15.5Ma为界,下部沉积物粘土矿物组成中蒙脱石含量高达70%,上部则以伊利石和绿泥石逐步增高、蒙脱石含量明显下降为特征,揭示出该区深海沉积物中粘土矿物演变可以分为32.8~15.5Ma的构造控制期和15.5Ma以来的气候控制期。在构造控制期,粘土矿物成分记录了南海扩张演变的历史;而在气候控制期,粘土矿物特征除反映出南海北部周边总体降温的过程外,还显示了3Ma的突然降温,与该站底栖有孔虫氧同位素资料反映的全球气候变化具有很好的对比性。

    English Abstract

    唐松, 邵磊, 赵泉鸿. 南海渐新世以来粘土矿物的演变特征及意义[J]. 沉积学报, 2004, 22(2): 337-342.
    引用本文: 唐松, 邵磊, 赵泉鸿. 南海渐新世以来粘土矿物的演变特征及意义[J]. 沉积学报, 2004, 22(2): 337-342.
    TANG Song, SHAO Lei, ZHAO Quan-hong. Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance[J]. Acta Sedimentologica Sinica, 2004, 22(2): 337-342.
    Citation: TANG Song, SHAO Lei, ZHAO Quan-hong. Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance[J]. Acta Sedimentologica Sinica, 2004, 22(2): 337-342.
    参考文献 (29)

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