“Ultrahigh-temperature” metamorphism and titaniQ: Examples from eastern Siberia
- Авторы: Podlesskii K.K.1, Griboedova I.G.1, Kurdyukov E.B.1
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Учреждения:
- Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)
- Выпуск: Том 25, № 5 (2017)
- Страницы: 516-525
- Раздел: Article
- URL: https://journals.rcsi.science/0869-5911/article/view/177545
- DOI: https://doi.org/10.1134/S0869591117050058
- ID: 177545
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Аннотация
Titanium contents of quartz have been analyzed in samples of granulites from various metamorphic complexes of eastern Siberia (Sutam, Chogar, and Sharyzhalgai) that contain mineral assemblages conventionally regarded as indicative of “ultrahigh-temperature” metamorphism. The related TitaniQ temperature estimates (Wark and Watson, 2006) are consistent with those of other mineralogical geothermometers and are commonly much lower than “ultrahigh-temperature”.
Об авторах
K. Podlesskii
Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)
Автор, ответственный за переписку.
Email: kkp@igem.ru
Россия, Moscow, 119017
I. Griboedova
Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)
Email: kkp@igem.ru
Россия, Moscow, 119017
E. Kurdyukov
Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)
Email: kkp@igem.ru
Россия, Moscow, 119017
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