Composition of pore water and diagenetic carbonates of ODP Site 123-765
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Degradation of organic matter in slightly organic-rich (1 wt% organic carbon) Neogene calcareous turbidites of the Argo Basin at Site 765 by sulfate reduction results in...
阿尔戈海盆765站位处，有机碳含量为1 wt%的轻度富有机质新近纪钙质浊积岩中的有机质经硫酸盐还原作用发生降解，进而导致……
