ACCESSORY AND ROCK FORMING MINERALS MONITORING THE EVOLUTION OF ZONED MAFIC-ULTRAMAFIC COMPLEXES IN THE CENTRAL URAL MOUNTAINS

dc.contributor.authorKrause J.
dc.contributor.authorBrügmann G.E.
dc.contributor.authorPushkarev E.V.
dc.date.accessioned2026-10-19T05:22:00Z
dc.date.issued2007
dc.description.abstractThis study describes major and trace element compositions of accessory and rock forming minerals from three Uralian–Alaskan-type complexes in the Ural Mountains (Kytlym, Svetley Bor, Nizhnii Tagil) for the purpose of constraining the origin, evolution and composition of their parental melts. The mafic–ultramafic complexes in the Urals are aligned along a narrow, 900 km long belt. They consist of a central dunite body grading outward into clinopyroxenite and gabbro lithologies. Several of these dunite bodies have chromitites with platinum group element mineralization.
dc.identifierhttps://elibrary.ru/item.asp?id=13563675
dc.identifier.citationLithos, 2007, 95, 1-2, 19-42
dc.identifier.doi10.1016/j.lithos.2006.07.018
dc.identifier.issn0024-4937
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/55160
dc.subjectANKARAMITES
dc.subjectCHROMITITE
dc.subjectPARENTAL MELT
dc.subjectSPINEL
dc.subjectURAL MOUNTAINS
dc.subjectURALIAN-ALASKAN-TYPE COMPLEX
dc.titleACCESSORY AND ROCK FORMING MINERALS MONITORING THE EVOLUTION OF ZONED MAFIC-ULTRAMAFIC COMPLEXES IN THE CENTRAL URAL MOUNTAINS
dc.typeСтатья

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