与火山-热液作用有关的海洋天然气水合物

MARINE GAS HYDRATE RELATED TO VOLCANO-HYDROTHERMALISM

  • 摘要: 天然气水合物中烃类主要有生物成因和热解成因,然而随着水合物勘探开发的不断深入,分布于洋底、洋陆过渡带或拉张裂谷区与火山-热液作用有关的天然气水合物的发现则表明,海洋天然气水合物很可能存在第三种类型:无机成因天然气水合物。实验模拟表明,洋底岩石蛇纹石化可生成无机成因的天然气水合物,实际中我们在缺少沉积物的洋底和沉积物有机碳含量低(<0.5%~1.0%)的大陆边缘发现了与火山-热液有关的天然气水合物。因此,今后天然气水合物勘探开发中应特别重视寻找与火山-热液有关的天然气水合物。

     

    Abstract: Hydrocarbonin gas hydrate mainlyincludes biogenic and thermogenic gases.However,within-creasing understandings of gas hydrate,newevidences are coming to light that there exists inorganic gashydrate related with volcano-hydrothermalism,whichis discoveredin ocean floor,subduction zone or ex-tensional valley.Fieldinvestigations and laboratory si mulation have manifested that,seabed serpentiniza-tion could generate inorganic gases.In fact,we have found gas hydrate related with volcano-hydrother-malism whose sedi ments have thin thickness and low organic carbon quantity.Therefore,inorganic gashydrae deposits should be paid attention toin the future.

     

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