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emical behavior of elements at fossil sea floor water/sediment interface

机译:化石海底水/沉积物界面中元素的模拟行为

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This note deals with the geochemical behavior of elements near the water/sediment interface of a fossil seafloor. The Nandan-Hechi basin, located in northwest Guangxi, Southern China, is selected for exemplified study. It is an elongated basin, and devleoped on a Caledonian basement. Its Devonian strata host hydrotothermally sedimentary formations, and are typical of the intra-platformal basin facies sediments over southern CHina.
机译:本说明涉及化石海底水/沉积物界面附近元素的地球化学行为。研究选择了位于中国南部广西西北部的南丹河池盆地。它是一个细长的盆地,发育在喀里多尼亚基底上。它的泥盆纪地层是热液沉积的地层,是典型的中国南部台地盆地相沉积。

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