THE ULTRAMAFIC-MAFIC SECTION OF THE SOUTHERN BLOCK OF THE VOLKOV PLUTON (CENTRAL URALS): NEW DATA ON THE COMPOSITION OF AU-PD MINERALIZATION

dc.contributor.author	Anikina E.V.
dc.contributor.author	Rusin I.A.
dc.contributor.author	Pushkarev E.V.
dc.contributor.author	Knauf V.V.
dc.contributor.author	Garuti G.
dc.contributor.author	Zaccarini F.
dc.contributor.author	Bersenev S.Ya.
dc.date.accessioned	2022-08-03T05:21:02Z
dc.date.available	2022-08-03T05:21:02Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13467671
dc.identifier.citation	Doklady Earth Sciences, 2004, 396, 4, 546-550
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38480
dc.description.abstract	The Au-Pd mineralization in olivine gabbros of the southern concentric block of the Volkov Pluton is controlled by inhomogeneous taxitic clinopyroxenite, wehrlite, and olivinite zones that, probably, formed in the presence of fluid under nonstationary dynamic conditions. Appreciable mineralogical distinctions of noble metals mineralization in various rocks, on the one hand and similar concentrations and proportions of noble metals, on the other hand, indicate local variations in the crystallization condition of noble metals minerals because of fluid-matrix interaction during subsolidus cooling of the host rocks.
dc.title	THE ULTRAMAFIC-MAFIC SECTION OF THE SOUTHERN BLOCK OF THE VOLKOV PLUTON (CENTRAL URALS): NEW DATA ON THE COMPOSITION OF AU-PD MINERALIZATION
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.