Инд. авторы:	Korsakov A.V.
Заглавие:	Application of raman imaging in UHPM research
Библ. ссылка:	Korsakov A.V. Application of raman imaging in UHPM research // Springer Series in Surface Sciences. - 2018. - Vol.66. - P.237-258.
Идентиф-ры:	DOI: 10.1007/978-3-319-75380-5_11; РИНЦ: 35490371; SCOPUS: 2-s2.0-85043253768; WoS: 000459495500013;
Реферат:	eng: Crustal-derived rocks can be subducted to mantle depth and metamorphosed at ultra-high pressure conditions (>2.6 GPa and 600 ∘ C), which are defined by the presence of coesite. Findings of diamond in metamorphic rocks further extended the upper pressure limit for crustal rocks (>4.0 GPa and 900–1000 ∘ C). Almost all ultra-high pressure mineral-indicators occur as small relics and Raman spectroscopy is a very powerful tool for the identification of these relics. Despite the significant progress in Raman imaging, this technique remains underestimated in ultra-high pressure research. In this chapter several examples of Raman imaging applied in ultra-high pressure petrology are summarised and discussed. © Springer International Publishing AG 2018.
Ключевые слова:	AQUEOUS FLUIDS; DIAMOND FORMATION; BEARING CLINOPYROXENE; FLUID INCLUSIONS; DEEP FLUIDS; CALC-SILICATE ROCKS; COESITE-QUARTZ TRANSITION; PRESSURE METAMORPHIC ROCKS; KOKCHETAV MASSIF; WESTERN ALPS;
Издано:	2018
Физ. хар-ка:	с.237-258
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