Liquidus thermobarometer for chromite–melt equilibrium modeling: Development and verification
- 作者: Aryaeva N.1, Koptev-Dvornikov E.2, Bychkov D.2
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隶属关系:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Moscow State University
- 期: 卷 71, 编号 5 (2016)
- 页面: 337-346
- 栏目: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174298
- DOI: https://doi.org/10.3103/S0145875216050021
- ID: 174298
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详细
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.
作者简介
N. Aryaeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
编辑信件的主要联系方式.
Email: aryana_@mail.ru
俄罗斯联邦, Staromonetnyi per. 35, Moscow, 119017
E. Koptev-Dvornikov
Moscow State University
Email: aryana_@mail.ru
俄罗斯联邦, Moscow, 119997
D. Bychkov
Moscow State University
Email: aryana_@mail.ru
俄罗斯联邦, Moscow, 119997