Open AccessEvolution of mineral formation processes in Lower Vend terrigenous rocks of Nepsko-Botuobinskaya anteclise
Author(s) -
А. В. Постников,
А. В. Постников,
О. В. Постникова,
О. В. Постникова,
E. S. Izyurova,
Е С Изъюрова,
V. V. Poshibaev,
V. V. Poshibaev,
А. С. Кузнецов,
А. С. Кузнецов,
A. D. Iz”yurov,
А Д Изъюров,
А. Е. Козионов,
А. Е. Козионов
Publication year - 2019
Publication title -
litologiâ i poleznye iskopaemye
Language(s) - English
Resource type - Journals
ISSN - 0024-497X
DOI - 10.31857/s0024-497x2019131-43
Subject(s) - terrigenous sediment , geology , geochemistry , mineral , cataclastic rock , diagenesis , magmatism , paleontology , sedimentary rock , tectonics , chemistry , organic chemistry
Principal common factors of epigenetic occurrence in Lower Vend rocks of Nepsko-Botuobinskaya anteclise are shown in the article. Evolution of mineral formation processes is stated in the change of mineral paragenesis, which were formed on stages of regional background (stadial) lithogenesis of foundering — diagenesis, early and late katagenesis; and also as a result of local superimposed lithogeneous types complex combination – cataclastic, hydrothermal, metasomatic and dynamothermal activation. Local superimposed processes could acompony the period of Permo-Triassic trap magmatism. High degree transformation of Lower Vend terrigenous rocks of Nepsko-Botuobinskaya anteclise determinates its structure, composition and physical properties specificity, which should be taken into account in process of geological exploration of different mineral deposits.