Marine gas hydrate is a great potential energy source.
海洋天然气水合物是一种潜在的巨大能源。
Marine gas hydrate, potential fossil energy resources, has attracted more and more attention.
作为一种极有潜力的化石能源-海洋天然气水合物日益受到人们更多的关注。
The seeping methane results in a special geological chemical micro-environment in marine gas hydrate geologic system.
在海洋天然气水合物的地质系统中，甲烷的渗漏作用形成了独特的地球化学微环境。
On the basis of some experimental research, it is recently proved that the method can also be applied to marine gas hydrate prospecting.
近几年通过对海底天然气水合物地球化学勘查试验研究，发现该方法也能应用其中。
The elemental geochemical anomaly of pore water in Marine sediments during the formation of gas hydrate is a significant indication for Marine gas hydrates in the deep sea floor.
海洋天然气水合物在生成过程中会引起周围沉积物孔隙水中元素地球化学异常，这些异常是指示天然气水合物存在的重要标志。
Besides temperature and pressure, the controlling factors for gas hydrate stability also include pore water composition, gas concentration in the fluid and Marine sediment types in the seafloor.
海洋天然气水合物的生成除了受温度和压力的影响外，还要受到孔隙水的化学组成、流体中气体的浓度及沉积物类型的影响。
Gas hydrate is a very important Marine energy in the future.
海洋水合物是未来的新型海洋天然气能源。
The effect of porous sediments, composition of pore water on formation conditions of natural gas hydrates was investigated. Natural gas hydrate formation in marine sediments was also discussed.
文章探讨了多孔沉积物、孔隙水成分等因素对天然气水合物形成条件的影响，分析了海底天然气水合物的成藏特性。
The effect of porous sediments, composition of pore water on formation conditions of natural gas hydrates was investigated. Natural gas hydrate formation in marine sediments was also discussed.
文章探讨了多孔沉积物、孔隙水成分等因素对天然气水合物形成条件的影响，分析了海底天然气水合物的成藏特性。
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