Origin and composition of fluid responsible for metasomatic processes in shear zones of the Bolshie Keivy tectonic nappe, baltic shield: Carbon isotope composition of graphite

Based on the analysis of parageneses and thermo dynamic calculations, we determined the physico chemical conditions of the formation of metasomatites and host metamorphic rocks.

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Bibliographic Details
Published in:	Doklady earth sciences Vol. 438; no. 1; pp. 701 - 704
Main Authors:	Bushmin, S. A., Glebovitskii, V. A., Prasolov, E. M., Lokhov, K. I., Vapnik, E. A., Savva, E. V., Shcheglova, T. P.
Format:	Journal Article
Language:	English
Published:	Dordrecht SP MAIK Nauka/Interperiodica 01-05-2011 Springer Springer Nature B.V
Subjects:	Carbon isotopes Cratons Earth and Environmental Science Earth Sciences Geochemistry Graphite Metamorphic rocks Petrology Tectonics (Geology) Europe, Baltic Shield Carbon Isotope Composition DOKLADY Earth Science Fluid Inclusion Shear Zone Kyanite
Online Access:	Get full text
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Description
Summary:	Based on the analysis of parageneses and thermo dynamic calculations, we determined the physico chemical conditions of the formation of metasomatites and host metamorphic rocks.
Bibliography:	ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23
ISSN:	1028-334X 1531-8354
DOI:	10.1134/S1028334X11050308