孟明, 尹维翰, 龚建明, 何拥军, 廖晶. 印度专属经济区天然气水合物的主控因素[J]. 海洋地质前沿, 2018, 34(6): 44-49. DOI: 10.16028/j.1009-2722.2018.06006
    引用本文: 孟明, 尹维翰, 龚建明, 何拥军, 廖晶. 印度专属经济区天然气水合物的主控因素[J]. 海洋地质前沿, 2018, 34(6): 44-49. DOI: 10.16028/j.1009-2722.2018.06006
    MENG Ming, YIN Weihan, GONG Jianming, HE Yongjun, LIAO Jing. DISCUSSION ON MAIN CONTROL FACTORS OF GAS HYDRATE IN INDIAN EXCLUSIVE ECONOMIC ZONES[J]. Marine Geology Frontiers, 2018, 34(6): 44-49. DOI: 10.16028/j.1009-2722.2018.06006
    Citation: MENG Ming, YIN Weihan, GONG Jianming, HE Yongjun, LIAO Jing. DISCUSSION ON MAIN CONTROL FACTORS OF GAS HYDRATE IN INDIAN EXCLUSIVE ECONOMIC ZONES[J]. Marine Geology Frontiers, 2018, 34(6): 44-49. DOI: 10.16028/j.1009-2722.2018.06006

    印度专属经济区天然气水合物的主控因素

    DISCUSSION ON MAIN CONTROL FACTORS OF GAS HYDRATE IN INDIAN EXCLUSIVE ECONOMIC ZONES

    • 摘要: 印度国家天然气水合物计划(NGHP-01)于2006年在克里希纳—戈达瓦里河(KG)盆地、曼哈纳迪盆地、安德曼海盆地、喀拉拉—康坎(KK)盆地实施,除KK盆地外均获得了水合物样品。为了探讨上述4个盆地天然气水合物的主控因素,较全面地收集、整理、比较了各个盆地的沉积背景、沉积速率、沉积物厚度、总有机碳(TOC)含量以及水合物钻探情况,发现KG盆地沉积物厚度最大,有机质含量最高,同时水合物饱和度较大,而KK盆地沉积物厚度最小、有机质含量最低,未钻获水合物样品,曼哈纳迪盆地和安德曼海盆地的沉积物厚度、有机质含量及水合物饱和度介于中间。结合我国南海水合物的钻探实际,可以认为沉积物厚度和有机质含量对印度专属经济区天然气水合物具有重要的控制作用。

       

      Abstract: The Indian National Gas Hydrate Program Expedition 01 (NGHP-01) was executed in 2006 in the Krishna-Godavari(KG) Basin, Mahanadi Basin, Andaman Sea and Kerala-Konkan (KK) Basin. Hydrate samples were obtained from all these basins except for the KK Basin. In order to study the main controlling factors on gas hydrate in the four basins mentioned above, data of sedimentary background, including sedimentation rate, sediment thickness, total organic carbon (TOC) content in addition to the information on hydrate drilling are collected and compared. The KG Basin is the basin with largest sediment thickness and highest organic matter, and the hydrate saturation is relatively high; while the KK Basin is the basin with smallest sediment thickness and lowest organic matter, and no hydrate samples have been collected so far. Comparing with what we learnt from the South China Sea, it is concluded that sediment thickness and organic matter content have important control over gas hydrates occurrence in the Indian Exclusive Economic Zones.

       

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