A Liquidus Thermobarometer for Modeling of the Magnetite–Melt Equilibrium
- Авторы: Aryaeva N.1, Koptev-Dvornikov E.2, Bychkov D.2
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Учреждения:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Department of Geology
- Выпуск: Том 73, № 2 (2018)
- Страницы: 177-186
- Раздел: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174672
- DOI: https://doi.org/10.3103/S0145875218020023
- ID: 174672
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Аннотация
A liquidus thermobarometer for the magnetite–silicate melt equilibrium was obtained by processing of a sample of 93 experimental equilibria of magnetite with basic melts using the methods of multidimensional statistics. The equations reproduce experimental data in a wide range of basic compositions, temperatures, and pressures with low error. Verification of the thermobarometers shows that the maximum error in liquidus temperature reproduction does not exceed ±7°C. The level of cumulative magnetite in the vertical sections of the Tsypringa, Kivakka, and Burakovskii intrusions is predicted with errors from ±10 to ±50 m.
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N. Aryaeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Автор, ответственный за переписку.
Email: aryana_@mail.ru
Россия, Moscow, 119017
E. Koptev-Dvornikov
Department of Geology
Email: aryana_@mail.ru
Россия, Moscow, 119991
D. Bychkov
Department of Geology
Email: aryana_@mail.ru
Россия, Moscow, 119991