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海相沉积中稳定硫同位素~(32)S 和~(34)S 的分布能够揭示硫酸盐、H_2S 和硫化铁的来源以及成岩过程。为此,BO BAR—KER JRGENSEN 用硫循环的扩散—成岩理论,建立了一种可用来计算
The distribution of stable sulfur isotopes ~ (32) S and ~ (34) S in marine sediments can reveal the source and diagenesis of sulfate, H 2 S and iron sulfide. To this end, BO BAR-KER JRGENSEN uses a diffusion-diagenetic theory of sulfur cycles to establish a method that can be used to calculate