Liquidus thermobarometer for chromite–melt equilibrium modeling: Development and verification
- Authors: Aryaeva N.S.1, Koptev-Dvornikov E.V.2, Bychkov D.A.2
-
Affiliations:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Moscow State University
- Issue: Vol 71, No 5 (2016)
- Pages: 337-346
- Section: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174298
- DOI: https://doi.org/10.3103/S0145875216050021
- ID: 174298
Cite item
Abstract
Liquidus chromite–silicate melt thermobarometer has been calculated by multiple linear regression of 234 experimental chromite–mafic melt equilibriums. Equations with low error reproduce the experimental compositions in a wide range of the compositions of mafic rocks, temperature, and pressure. Verification of the thermobarometers showed that the maximum error of the reproduction of the liquidus temperature is less than ±12°C. The formation equation of the cumulative chromites in the vertical section of the Burakovskii pluton was predicted with an error of ±50 m.
Keywords
About the authors
N. S. Aryaeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Author for correspondence.
Email: aryana_@mail.ru
Russian Federation, Staromonetnyi per. 35, Moscow, 119017
E. V. Koptev-Dvornikov
Moscow State University
Email: aryana_@mail.ru
Russian Federation, Moscow, 119997
D. A. Bychkov
Moscow State University
Email: aryana_@mail.ru
Russian Federation, Moscow, 119997