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- W2333859491 abstract "Confocal Raman Imaging revealed the coexistence of kokchetavite and K-cymrite (KAlSi 3 O 8 ·H 2 O) in association with muscovite/phengite, lollingite, calcite and α-cristobalite in polyphase mineral inclusions in clinopyroxene of calc-silicate ultrahigh-pressure metamorphic (UHPM) rocks from the Kokchetav Complex (northern Kazakhstan). Experiments have shown that K-cymrite is stable under high pressure conditions; however, this phase never had been reported from UHPM rocks before. The mode of occurrence of K-cymrite and kokchetavite in these rocks is strong evidence for kokchetavite formation through the dehydration of K-cymrite. The presence of fluid inclusions and K-cymrite in the polyphase mineral inclusions testify for water-saturated conditions in the rock-forming environment near peak metamorphic conditions." @default.
- W2333859491 created "2016-06-24" @default.
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- W2333859491 date "2014-01-16" @default.
- W2333859491 modified "2023-10-01" @default.
- W2333859491 title "Origin of K-cymrite and kokchetavite in the polyphase mineral inclusions from Kokchetav UHP calc-silicate rocks: evidence from confocal Raman imaging" @default.
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- W2333859491 doi "https://doi.org/10.1127/0935-1221/2013/0025-2321" @default.
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