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冷泉碳酸盐岩
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冷泉碳酸盐岩
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cold seep carbonate
冷泉碳酸盐岩
冷泉流体由深部向上渗漏过程中,在海底附近经甲烷氧化古细菌和硫酸盐还原细菌共同作用下发生缺氧甲烷氧化反应引起环境碱度的升高从而形成的沉淀物质。
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