Mineral-petrographic and geochemical features of conglomerates of the Belokataisk formation, conditions of formation and their minergenia

Authors

  • Artyom Konstantinovich Trutnev Ural State Mining University
  • Evgeny Alexandrovich Zhuklin Ural State Mining University
  • D.I. Prokopchuk Ural State Mining University
  • Lyubov Andreevna Demina Ural State Mining University

DOI:

https://doi.org/10.17072/chirvinsky.2022.271

Keywords:

sedimentary rocks, belokataiskaya suite, conglomerates, petrochemical modules, geochemistry, geodynamics, gold

Abstract

In the geological history of the Earth, conglomerates are found in a variety of formations, including platform and geosynclinal formations, in molasse strata of intermontane depressions, foredeeps, etc. A detailed analysis of conglomerates makes it possible to identify the facies (formational) belonging of sedimentary deposits, their place in the history of geological development, mineralogical, petrographic and geochemical features, which ultimately leads to the identification of metallogenic specialization of specific sedimentary strata.

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Published

2022-04-12

How to Cite

Trutnev А. К., Zhuklin Е. А., Prokopchuk Д., & Demina Л. А. (2022). Mineral-petrographic and geochemical features of conglomerates of the Belokataisk formation, conditions of formation and their minergenia. Problems of Mineralogy, Petrography and Metallogeny. Scientific Readings in Memory of P.N. Chirvinsky, (25), 271–277. https://doi.org/10.17072/chirvinsky.2022.271

Issue

No. 25 (2022): Readings in memory of P.N. Chirvinsky 2022

Section

Статьи