Year: 2018
Pages: 98-108
UDC: 55(47+57)
Number: 3
Type: scientific article
DOI: http://doi.org/10.31084/2619-0087/2018-3-7
Topic: ARTICLES AND PUBLICATIONS
Authors: Kovalev, Sergei G., Kovalev, Sergei S., Vysotsky, Sergei I.
The paper presents new data on the conditions of formation of igneous rocks in the western slope of the Southern Urals and the adjacent part of the East European platform. Calculations of P-T mantle melting parameters show that the implementation of plume process results in formation of one-type rocks (picrites and picrodolerites), but their genesis may be fundamentally different. One kind is the result of crystallization of undifferentiated mantle melt in the upper layers of the crust, while the other is formed by differentiation in large intracrustal magma chambers.
plume, magmatic melt, P-T parameters of picrites, picrodolerites, the western slope of the Southern Urals, differentiation, olivine, pyroxene geothermometer, Middle Riphean