Bedrock platinum-group element mineralization of zonal clinopyroxenite–dunite massifs of the Middle Urals
- Authors: Malitch K.N.1, Stepanov S.Y.1, Badanina I.Y.1, Khiller V.V.1
-
Affiliations:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Issue: Vol 476, No 2 (2017)
- Pages: 1147-1151
- Section: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/191022
- DOI: https://doi.org/10.1134/S1028334X17100051
- ID: 191022
Cite item
Abstract
Features of the chemical composition of platinum-group mineral assemblages from chromitites of the zonal Svetly Bor, Veresovy Bor, and Nizhny Tagil clinopyroxenite–dunite massifs of the Middle Urals are compared for the first time.
About the authors
K. N. Malitch
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Author for correspondence.
Email: dunite@yandex.ru
Russian Federation, Yekaterinburg, 620016
S. Yu. Stepanov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: dunite@yandex.ru
Russian Federation, Yekaterinburg, 620016
I. Yu. Badanina
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: dunite@yandex.ru
Russian Federation, Yekaterinburg, 620016
V. V. Khiller
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: dunite@yandex.ru
Russian Federation, Yekaterinburg, 620016
Supplementary files
