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一简要回顾北京大学郑淑惠指出:“古代碳酸盐岩的地质应用,只有解决了矿物同位素数据的保存性问题,才能更好地阐明地质过程”。很多地球化学家研究现代、亚近代和古代沉积时,不但研究全岩,而且研究沉积物组份、胶结物和各种生物化石的碳、氧稳定同位素组成,并且进行彼此间的对比,进而探讨矿物岩石同位素变化规律和地质应用。罗宾·巴瑟斯特(1977)主要依据Grose,Friedman,Land和Choguette的资料,全面地总结了现代和亚近代沉积方面的
A brief review of Zheng Shuhui Peking University pointed out: “The geological application of the ancient carbonate rock, only to solve the conservation of mineral isotope data problems in order to better clarify the geological process.” Many geochemists have studied not only whole rocks but also carbon and oxygen stable isotopic compositions of sediment components, cements, and various biological fossils when studying modern, sub-modern, and ancient sediments, and then conducted a comparison with each other Mineral Rock Isotope Variation and Geological Applications. Robin Bathurst (1977), based largely on the data of Grose, Friedman, Land and Choguette, provides a comprehensive summary of modern and sub-modern sedimentation