Fluid inclusions in rock-forming minerals of ultrahigh-pressure metamorphic rocks (Kokchetav massif, Northern Kazakhstan)

A study presents original data on the composition of fluid inclusions in garnets and clinopy roxenes from high pressure garnetclinopyroxene rocks of the Kokchetav massif (Northern Kazakh stan). The presence of secondary fluid inclusions in fractures cutting all growth zones of garnet crystals provid...

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Bibliographic Details
Published inDoklady earth sciences Vol. 437; no. 2; pp. 473 - 478
Main Authors Korsakov, A. V., Golovin, A. V., Dieing, T., Toporski, J.
Format Journal Article
LanguageEnglish
Published Dordrecht SP MAIK Nauka/Interperiodica 01.04.2011
Springer
Springer Nature B.V
Subjects
Crystallization
Crystals
Earth and Environmental Science
Earth Sciences
Fluid dynamics
Geochemistry
High pressure
Metamorphic rocks
Metamorphism
Mineralogy
Rocks, Metamorphic
Thermodynamics
Kazakhstan
Primary Fluid Inclusion
Fluid Inclu
Host Mineral
DOKLADY Earth Science
Fluid Inclusion
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Summary:A study presents original data on the composition of fluid inclusions in garnets and clinopy roxenes from high pressure garnetclinopyroxene rocks of the Kokchetav massif (Northern Kazakh stan). The presence of secondary fluid inclusions in fractures cutting all growth zones of garnet crystals provides evidence for the fact that hydrous fluid played an important role in one of the final stages of retrograde metamorphism.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
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ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X11040040