Year: 2021
Pages: 3-16
UDC: 551.251+551.8
Number: 2
Type: scientific article
DOI: 10.31084/2619-0087/2021-2-1
Topic: ARTICLES AND PUBLICATIONS
Authors: Snachev, Akexander V., Snachev, Vladimir I.
The Kyshtym (PR1 kš), Saitovo (RF2st), Igish (RF2ig), and Kundravi (Vkn) Formations are distributed within the framework of the Ilmen metamorphic complex and envelop the Chashkov granite massif and the Elanchik antiform structure in a narrow strip. Geological, petrochemical, and thermobarometric data on biotite-garnet and amphibole-garnet parageneses and carbonaceous shales made it possible to conclude that the black shale deposits of the above formations were formed in the distal deep-water environment and remote from the coastline area of the sedimentary basin. They belong to the low-carbonaceous and carbonaceous types, as well as the siliceous-carbonaceous formation, which has a minimum amount of terrigenous impurities in its composition. At the boundary between the Riphean and Vendian, when a major structural transformation occurred in the Southern Urals, volcanogenic-sedimentary rocks of the above formations experienced regional metamorphism under conditions of the epidote-amphibolite facies (T = 470–580°C, P = 2.0–7.2 kbar , abyssal depth zone). Later, during the formation of the large Argazi, Kisegach, Elanchik and Chashkov granitoid massifs, the deposits of the Ilmen-Sysert anticlinorium underwent zonal contact metamorphism. Depending on the distance to acidic intrusions, they underwent transformation under conditions from the facies of almandine amphibolites (T = 750–770°C, P = 8.8–9.0 kbar) to cummingtonite amphibolites (T = 530–550°C, P = 2.1–3.6 kbar).
Ilmen-Sysert anticlinorium, Saitovo Series, Kyshtym Series, Kundravi Series, Igish Series, temperature, pressure, paleogeography, paleogeodynamics