“Ultrahigh-temperature” metamorphism and titaniQ: Examples from eastern Siberia
- 作者: Podlesskii K.K.1, Griboedova I.G.1, Kurdyukov E.B.1
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隶属关系:
- Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)
- 期: 卷 25, 编号 5 (2017)
- 页面: 516-525
- 栏目: Article
- URL: https://journals.rcsi.science/0869-5911/article/view/177545
- DOI: https://doi.org/10.1134/S0869591117050058
- ID: 177545
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详细
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”.
作者简介
K. Podlesskii
Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)
编辑信件的主要联系方式.
Email: kkp@igem.ru
俄罗斯联邦, Moscow, 119017
I. Griboedova
Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)
Email: kkp@igem.ru
俄罗斯联邦, Moscow, 119017
E. Kurdyukov
Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM)
Email: kkp@igem.ru
俄罗斯联邦, Moscow, 119017
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