Stable isotope (C, O, H) characteristics and genesis of the Tazheran brucite marbles and skarns, Olkhon region, Russia › Research Explorer

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Stable isotope (C, O, H) characteristics and genesis of the Tazheran brucite marbles and skarns, Olkhon region, Russia

Research output: Contribution to journal › Article › peer-review

DOI

https://doi.org/10.1007/s00710-016-0477-8
Final published version

Anna Doroshkevich
Eugene Sklyarov
Anastasia Starikova
Vladimir Vasiliev
German Ripp
Ivan Izbrodin
Viktor Posokhov

Original language	English
Pages (from-to)	399-416
Number of pages	18
Journal	Mineralogy and Petrology
Volume	111
Issue number	3
DOIs	https://doi.org/10.1007/s00710-016-0477-8
Publication status	Published - 1 Jun 2017

Research areas

Brucite marble, Decarbonation, Fluid depleted in C, Fluid-rock interaction, Olkhon collision system, Skarn, Stable isotopes, Tazheran gabbro-syenite massif, CONTACT-METAMORPHISM, SYSTEM, Skam, FRACTIONATION, MINERALS, INTRUSION, SELF-ORGANIZATION, OXYGEN, BAIKAL REGION, Fluid depleted in C-13, CARBONATE, WALL ROCK

OECD FOS+WOS

ID: 10321190