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南海东北部甲烷成因碳酸盐岩的矿物学及同位素组成

陆红锋 陈芳 刘坚 周洋 廖志良

陆红锋, 陈芳, 刘坚, 周洋, 廖志良. 南海东北部甲烷成因碳酸盐岩的矿物学及同位素组成[J]. 海洋地质与第四纪地质, 2010, 30(2): 51-59. doi: 10.3724/SP.J.1140.2010.02051
引用本文: 陆红锋, 陈芳, 刘坚, 周洋, 廖志良. 南海东北部甲烷成因碳酸盐岩的矿物学及同位素组成[J]. 海洋地质与第四纪地质, 2010, 30(2): 51-59. doi: 10.3724/SP.J.1140.2010.02051
LU Hongfeng, CHEN Fang, LIU Jian, ZHOU Yang, LIAO Zhiliang. Mineralogies and Stable Isotopic Compositions of Methane-derived Carbonates from the Northeastern South China Sea[J]. Marine Geology & Quaternary Geology, 2010, 30(2): 51-59. doi: 10.3724/SP.J.1140.2010.02051
Citation: LU Hongfeng, CHEN Fang, LIU Jian, ZHOU Yang, LIAO Zhiliang. Mineralogies and Stable Isotopic Compositions of Methane-derived Carbonates from the Northeastern South China Sea[J]. Marine Geology & Quaternary Geology, 2010, 30(2): 51-59. doi: 10.3724/SP.J.1140.2010.02051

南海东北部甲烷成因碳酸盐岩的矿物学及同位素组成


doi: 10.3724/SP.J.1140.2010.02051
详细信息
    作者简介:

    LU Hongfeng,male,born in 1976,Ph.D.,mainly focus on Petrography and Mineralogy,E-mail:luhongfeng@hydz.cn

  • 中图分类号: P736.4

Mineralogies and Stable Isotopic Compositions of Methane-derived Carbonates from the Northeastern South China Sea

More Information
  • 摘要: 取自南海北部的3块自生碳酸盐岩主要为圆环状、结核状和结壳状。X射线衍射分析显示,这3件碳酸盐岩主要由黏土矿物、陆源碎屑(石英、长石)和碳酸盐矿物(高镁方解石和铁白云石)组成;碳氧同位素分析表明,结核状和结壳状碳酸盐岩具有极负的δ13C (分别为-32.83‰和-38.01‰PDB)和正的δ18O (分别为+2.19‰和+2.96‰PDB),不同于正常沉积的海相碳酸盐岩,甲烷厌氧氧化过程控制了这些碳酸盐岩的形成。碳酸盐岩为甲烷成因,记录了南海东北部海底富含甲烷的冷泉活动历史。
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  • 收稿日期:  2009-06-05
  • 修回日期:  2009-08-28

南海东北部甲烷成因碳酸盐岩的矿物学及同位素组成

doi: 10.3724/SP.J.1140.2010.02051
    作者简介:

    LU Hongfeng,male,born in 1976,Ph.D.,mainly focus on Petrography and Mineralogy,E-mail:luhongfeng@hydz.cn

  • 中图分类号: P736.4

摘要: 取自南海北部的3块自生碳酸盐岩主要为圆环状、结核状和结壳状。X射线衍射分析显示,这3件碳酸盐岩主要由黏土矿物、陆源碎屑(石英、长石)和碳酸盐矿物(高镁方解石和铁白云石)组成;碳氧同位素分析表明,结核状和结壳状碳酸盐岩具有极负的δ13C (分别为-32.83‰和-38.01‰PDB)和正的δ18O (分别为+2.19‰和+2.96‰PDB),不同于正常沉积的海相碳酸盐岩,甲烷厌氧氧化过程控制了这些碳酸盐岩的形成。碳酸盐岩为甲烷成因,记录了南海东北部海底富含甲烷的冷泉活动历史。

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