Platinum-Group minerals as indicator of sulfur fugacity in ophiolitic upper mantle: an example from chromitites of the Ray-Iz ultramafic complex (Polar Urals, Russia)

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Platinum-Group minerals as indicator of sulfur fugacity in ophiolitic upper mantle: an example from chromitites of the Ray-Iz ultramafic complex (Polar Urals, Russia). / Garuti, Giorgio; Zaccarini, Federica; Moloshag, Vassili et al.
in: The Canadian Mineralogist, Jahrgang 37, 1999, S. 1099-1115.

Publikationen: Beitrag in FachzeitschriftArtikelForschung(peer-reviewed)

Bibtex - Download

@article{8ef1b0e85f7142d9ae87027fc7575e4d,
title = "Platinum-Group minerals as indicator of sulfur fugacity in ophiolitic upper mantle: an example from chromitites of the Ray-Iz ultramafic complex (Polar Urals, Russia)",
author = "Giorgio Garuti and Federica Zaccarini and Vassili Moloshag and Victor Alimov",
year = "1999",
language = "English",
volume = "37",
pages = "1099--1115",
journal = "The Canadian Mineralogist",
issn = "0008-4476",
publisher = "Mineralogical Association of Canada",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - Platinum-Group minerals as indicator of sulfur fugacity in ophiolitic upper mantle: an example from chromitites of the Ray-Iz ultramafic complex (Polar Urals, Russia)

AU - Garuti, Giorgio

AU - Zaccarini, Federica

AU - Moloshag, Vassili

AU - Alimov, Victor

PY - 1999

Y1 - 1999

M3 - Article

VL - 37

SP - 1099

EP - 1115

JO - The Canadian Mineralogist

JF - The Canadian Mineralogist

SN - 0008-4476

ER -