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科学界将深海中发现的热液露头和在近大陆地区发现的冷渗透气液归属为上世纪最后25年中最重要的发现。这些气液含有还原化合物,后者在微生物的参与下,或者通过化学途径发生氧化作用。这些作用过程在水—海底界面上和其附近海底表面以下形成了金属和非金属矿物的堆积并发生了显?
The discovery by the scientific community of the hydrothermal outcrops found in the deep ocean and the cold-infiltration gas and gas found in the near-mainland is the most important discovery of the last 25 years of the last century. These gas and liquid contain reducing compounds, the latter with the involvement of microorganisms, or by chemical means of oxidation. These processes formed and evolved the accumulation of metallic and non-metallic minerals below the seafloor surface at and near the water-seafloor interface.