Specific features of organic matter of clayy-anhydrite thickness of the Verkhnekamsky salt deposit

Authors

  • Boris Alexandrovich Bachurin Mining Institute of the Ural Branch of the Russian Academy of Sciences

DOI:

https://doi.org/10.17072/chirvinsky.2021.18

Keywords:

Verkhnekamsk salt deposit, subsalt deposits, bitumoids, IR spectroscopy, gas chro-matography-mass spectrometry, geochemical markers

Abstract

On the basis of the study of the core of the well No. 1119 of the Izversky area, the peculiarities of the composition of bitumoids of sulfate-carbonate-clay and clay-anhydrite strata of the subsalt part of the section of the Verkhne-Kama field are considered.

Author Biography

  • Boris Alexandrovich Bachurin , Mining Institute of the Ural Branch of the Russian Academy of Sciences

    Candidate of Geological and Mineralogical Sciences. Head of the Laboratory of Geoecology of Mining Regions, Mining Institute, Ural Branch of the Russian Academy of Sciences, Perm

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Published

2021-10-08

Issue

No. 24 (2021): Чтения памяти П.Н. Чирвинского 2021

Section

Статьи

How to Cite

Specific features of organic matter of clayy-anhydrite thickness of the Verkhnekamsky salt deposit. (2021). Problems of Mineralogy, Petrography and Metallogeny. Scientific Readings in Memory of P.N. Chirvinsky, 24, 18-24. https://doi.org/10.17072/chirvinsky.2021.18