OLIVINE-CHROMSPINEL OXYTHERMOBAROMETRY OF ULTRAMAFIC ROCKS OF THE ǏOKO-DOVYREN LAYERED MASSIF

dc.contributor.author	Pushkarev E.V.
dc.contributor.author	Votyakov S.L.
dc.contributor.author	Chashchukhin I.S.
dc.contributor.author	Kislov E.V.
dc.date.accessioned	2022-08-14T03:31:09Z
dc.date.available	2022-08-14T03:31:09Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13471160
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 2, 266-270
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38531
dc.description.abstract	Redox-condition of stratified ultramafite infusions is estimated by the modern methods of oxythermobarometry. Olivine-chromespinel equilibrium of ultramafites of the Ioko-Dovyrensk's stratified massive is studied. Temperature and fugacity of oxygen are evaluated on this basis at the instant of ending the exchange subsolidus reactions. Attempt is made to define the variations of fluid regime of rocks formation upon their interaction with the metasedimentary carbonate rocks.
dc.title	OLIVINE-CHROMSPINEL OXYTHERMOBAROMETRY OF ULTRAMAFIC ROCKS OF THE ǏOKO-DOVYREN LAYERED MASSIF
dc.type	Статья

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