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• W3141009711 abstract "学习显示在热水的液体有的海洋的地板的元素富人积极影响，不是仅仅在全部的器官的碳(TOC ) 上，而且在在一些的丰富 ofSiO_2 上中间上面原生地阶层。衣服与许多 SiO_2 忍受更好积极的关联。由在有机物和海地板之间的关联分析，热液体描绘了象 P 那样的微量元素， Gu， Zn， Ni， Ba，在海洋的碳酸盐岩的等等，我们断定碳酸盐岩的有机物丰富与海洋的地板有关在层的部分的热水的活动。一些薄分层的燧石，被认为是热水的活动的指示物，经常发生在 Gaoyuzhuang， Wumishan， Tieling 和 Xiamalingformation 支持我们的结论。与在海洋的碳酸盐岩增加微量元素， TOG 和 Fe/Ti 比率正在弄皱。相反， AI/(AI+Fe+Mn ) 比率通常正在减少。" @default.
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• W3141009711 date "2006-01-01" @default.
• W3141009711 modified "2023-09-23" @default.
• W3141009711 title "Influences of marine floor hydrothermal activity on organic matter abundance in marine carbonate rocks——A case study of middle-upper Proterozoic in the northern part of North China" @default.
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