Evolution of the Processes of Mineral Formation in Early Vendian Terrigenous Rocks of the Nepa–Botuoba Anteclise

Main regularities in the manifestation of epigenetic processes in Lower Vendian terrigenous rocks of the Nepa–Botuoba anteclise are established. Evolution of the processes of mineral formation is reflected in the sequential replacement of mineral assemblages formed at different stages of the regiona...

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Veröffentlicht in:Lithology and mineral resources 2019, Vol.54 (1), p.27-37
Hauptverfasser: Postnikov, A. V., Postnikova, O. V., Iz”yurova, E. S., Poshibaev, V. V., Kuznetsov, A. S., Iz”yuraov, A. D., Kozionov, A. E.
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container_end_page 37
container_issue 1
container_start_page 27
container_title Lithology and mineral resources
container_volume 54
creator Postnikov, A. V.
Postnikova, O. V.
Iz”yurova, E. S.
Poshibaev, V. V.
Kuznetsov, A. S.
Iz”yuraov, A. D.
Kozionov, A. E.
description Main regularities in the manifestation of epigenetic processes in Lower Vendian terrigenous rocks of the Nepa–Botuoba anteclise are established. Evolution of the processes of mineral formation is reflected in the sequential replacement of mineral assemblages formed at different stages of the regional background lithogenesis related to subsidence: diagenesis, early and late catagenesis, as well as superimposement of local processes (cataclastic, hydrothermal-metasomatic, and dynamothermal activation) probably related to the Permo-Triassic trap magmatism. High degree of the alteration of Early Vendian terrigenous rocks in the Nepa–Botuoba anteclise is responsible for their specific texture, composition, and physical properties that should be taken into consideration during geological explorations aimed at prospecting for various mineral resources.
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Earth Sciences
Mineral Resources
Mineralogy
Sedimentology
title Evolution of the Processes of Mineral Formation in Early Vendian Terrigenous Rocks of the Nepa–Botuoba Anteclise
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