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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Bibliographic Details
Main Authors: D.E. Saveliev, E.V. Belogub, I.A. Blinov, D.A. Kozhevnikov, V.A. Kotlyarov
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2016-12-01
Series:Минералогия
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Online Access:https://journal.mineralogy.ru/wp-content/uploads/2019/09/2016-4-5.pdf
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