The Composition of Mica from the Salmi Batholith Granites as an Indicator of the Formation of Nb–Ta Mineralization
- Authors: Konyshev A.A.1,2, Alferyeva Y.O.3, Anosova M.O.1, Rusak A.A.1, Korepanov Y.I.2
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Affiliations:
- Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
- Korzhinskii Institute of Experimental Mineralogy, Russian Academy of Sciences
- Department of Geology, Moscow State University
- Issue: Vol 74, No 4 (2019)
- Pages: 401-411
- Section: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/175022
- DOI: https://doi.org/10.3103/S0145875219040045
- ID: 175022
Cite item
Abstract
Successive differentiates of acid rocks from the Salmi batholith are represented by the following series: biotite–amphibole rapakivi granite, biotite granite, and highly differentiated granites (Li-siderophyllite and Li–F zinnwaldite varieties). There is a gradual increase in the content of Ta and Nb and a decrease in the Nb/Ta ratio in this rock series. A regular change in the Ta and Nb partitioning coefficients between mica and the bulk rock composition is observed as well. Comparison of Li-siderophyllite granite and Li–F granite shows that the latter has a sharp decrease in the partitioning coefficients KpTa, Nb. This is due to a decrease in the content of these metals in zinnwaldite from Li–F granite and associates with the appearance of columbite in these rocks. The study of rock samples from the Salmi batholith suggests that such change of the Ta and Nb content in the mica from deeply differentiated granite and the corresponding decrease in the Kp value of these metals may be diagnostic evidence of the presence of columbite mineralization in the rock.
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About the authors
A. A. Konyshev
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences; Korzhinskii Institute of Experimental Mineralogy, Russian Academy of Sciences
Author for correspondence.
Email: icelopa@gmail.com
Russian Federation, Moscow, 119991; Chernogolovka, Moscow oblast, 142432
Ya. O. Alferyeva
Department of Geology, Moscow State University
Author for correspondence.
Email: YanaAlf@ya.ru
Russian Federation, Moscow, 119991
M. O. Anosova
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
Author for correspondence.
Email: masha_anosova@mail.ru
Russian Federation, Moscow, 119991
A. A. Rusak
Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
Author for correspondence.
Email: aleks7975@yandex.ru
Russian Federation, Moscow, 119991
Ya. I. Korepanov
Korzhinskii Institute of Experimental Mineralogy, Russian Academy of Sciences
Author for correspondence.
Email: yakoff@iem.ac.ru
Russian Federation, Chernogolovka, Moscow oblast, 142432