PETROLOGICAL EVIDENCES OF SYNDEFORMATION SEGREGATION OF CHROMITES DURING DUNITE FORMATION: EXAMPLE OF KRAKA OPHIOLITES, SOUTH URALS

Results of structural and mineralogical studies of chromitite-bearing zone localized in spinel peridotites of the Middle Kraka ophiolite massif are presented. The rocks of the studied area are characterized by deformation structures, which are cuased by plastic flow under high-PT conditions. Olivine...

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Главные авторы:	D.E. Saveliev, E.V. Belogub, I.A. Blinov, D.A. Kozhevnikov, V.A. Kotlyarov
Формат:	Artigo
Язык:	Inglês
Опубликовано:	South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2016-12-01
Серии:	Минералогия
Предметы:	mantle ultramafic rocks cr deposits plastic deformation olivine chromite segregation coalescense kraka south urals
Online-ссылка:	https://journal.mineralogy.ru/wp-content/uploads/2019/09/2016-4-5.pdf
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