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Sr-isotope Chemostratigraphy Of Carbonate Depositsfrom The Yenisei Group, Azyrtal Ridge,rneastern Slope Of Kuznetsk Alatau

机译:库兹涅茨克阿拉托东坡阿兹台尔岭叶尼塞集团碳酸盐矿床的锶同位素化学地层学

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This study uses Sr isotope chemostratigraphy to place constraints on the depositional age of carbonate rocks from the Yenisei Group, which are considered to be the Precambrian reference section in the western Altai-Sayan Folded Area. The least altered samples of carbonate rocks were selected on the basis of strict geochemical criteria, Mn/Sr_(0.2), Fe/Sr(5.0) for limestone and Mn/Sr_(1.0), Fe/Sr_(4.0) for dolomite. Preliminary leaching of samples in 1N solution of ammonium acetate was used to enrich these samples in primary carbonate matter. Sr chemostratigraphic signatures of carbonate deposits from the Yenisei Group revealed that deposition took place during the Late Vendian and Early Cambrian, in the time span of 580-530 Ma.
机译:这项研究使用Sr同位素化学地层学来限制叶尼塞组碳酸盐岩的沉积年龄,这些碳酸盐岩被认为是阿尔泰-萨彦岭褶皱地区西部的前寒武纪参考剖面。根据严格的地球化学标准选择了变化最小的碳酸盐岩样品,石灰石的Mn / Sr_(0.2),Fe / Sr(5.0)和白云岩的Mn / Sr_(1.0),Fe / Sr_(4.0)。样品在1N乙酸铵溶液中的初步浸出用于富集这些样品中的初级碳酸盐物质。来自叶尼塞集团的碳酸盐矿床的Sr化学地层学特征表明,沉积发生在Ventian晚期和Cambrian早期,时间跨度为580-530 Ma。

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