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首页> 外文期刊>Lithology and Mineral Resources >Isotope-geochemical features of Devonian rocks in the Pripyat Trough: Famennian suprasalt deposits
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Isotope-geochemical features of Devonian rocks in the Pripyat Trough: Famennian suprasalt deposits

机译:普里皮亚季槽泥盆纪岩石的同位素地球化学特征:法门尼超盐矿床

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摘要

This work presents the results of isotope studies of the Upper Devonian (Famennian) suprasalt complex carried out with core material of exploratory borehole 71 drilled at the northwestern margin of the Pripyat Trough. Lithological features of the rocks point to a high degree of postsedimentary transformation of rocks. Significant role in these transformations was played by evaporites and related brines and the presence of hydrocarbons in the sequence. Such a combination provides insight into the behavior of isotope systems under conditions of the geochemical transformation of sedimentary material. The combined application of several isotope (δ^sup 13^C, δ^sup 18^O, δ^sup 34^S, and ^sup 87^Sr/^sup 86^Sr) methods made it possible to consider the complex mechanisms of compositional and isotopic transformation of rocks in the course of their lithogenetic alterations. The source material can be deduced with a high probability from the Rb-Sr systematics of the clayey component of marls.[PUBLICATION ABSTRACT]
机译:这项工作介绍了在普里皮亚季槽西北边缘钻探性钻孔71的岩心材料进行的上泥盆统(法门尼)超盐岩同位素研究的结果。岩石的岩性特征表明岩石具有高度的沉积后转化作用。在这些转变中,蒸发物和相关的盐水以及序列中碳氢化合物的存在起着重要作用。这种组合提供了对沉积物地球化学转化条件下同位素系统行为的深入了解。几种同位素(δ^ sup 13 ^ C,δ^ sup 18 ^ O,δ^ sup 34 ^ S和^ sup 87 ^ Sr / ^ sup 86 ^ Sr)的组合应用使得可以考虑复杂的机理岩石成岩蚀变过程中岩石的组成和同位素转变可以从泥灰质黏土成分的Rb-Sr系统学中高度推断出源物质。[出版物摘要]

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