同时,地表下渗的大气降水携带了细菌类微生物,对原生有机质进行生物降解,并生成硫化氢类还原物质。
Moreover, the microorganism which was brought by permeable surface water degraded the primary kerogen in sedimantary rocks and could produce reducing matters. The precipitation and th…
同时,地表下渗的大气降水携带了细菌类微生物,对原生有机质进行生物降解,并生成硫化氢类还原物质。
Moreover, the microorganism which was brought by permeable surface water degraded the primary kerogen in sedimantary rocks and could produce reducing matters. The precipitation and th…
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