Тип публикации: статья из журнала
Год издания: 2017
Идентификатор DOI: 10.1002/jrs.5112
Ключевые слова: diamond anvil cell, high pressure, high temperature, Phengite, raman spectra
Аннотация: The in-situ method of Raman spectroscopy was used to study the layered mineral phengite, K(Al,Mg)2(Si,Al)4O10(OH)2, compressed in water under simultaneously high temperatures and pressures (respectively, up to 373 °S and 12.5 GPa). The implemented conditions were typical of modeling the 'cold' subduction zones in lithospheric slabs. The high pressures and temperatures were produced in an electrically heated diamond-anvil cell. Measured Raman spectra have demonstrated a high R-T stability of the mineral. No non-quenchable phengite states (no reversible or irreversible polymorphic transitions, overhydration or notable amorphization) were observed in the investigated samples.
Издание
Журнал: Journal of Raman Spectroscopy
ISSN журнала: 03770486
Издатель: John Wiley & Sons Ltd.
Персоны
- Goryainov S.V. (Sobolev Institute of Geology and Mineralogy SB RAS Academician Koptyug Avenue 3 Novosibirsk 630090 Russia)
- Polyansky O.P. (Sobolev Institute of Geology and Mineralogy SB RAS Academician Koptyug Avenue 3 Novosibirsk 630090 Russia)
- Krylov A.S. (Kirensky Institute of Physics SB RAS Akademgorodok Krasnoyarsk 660036 Russia)
- Vtyurin A.N. (Kirensky Institute of Physics SB RAS Akademgorodok Krasnoyarsk 660036 Russia)
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