Experimental Study of the Formation of Chromium-Bearing Priderite and Yimengite as Products of Modal Mantle Metasomatism

The results of experiments on the synthesis of exotic titanates (priderite and yimengite) simulating metasomatic conditions of alteration of the mantle minerals (chromite and ilmenite) are reported. Ba-free Cr-bearing priderite was synthesized for the first time. Experiments showed the possibility o...

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Bibliographic Details
Published in:Doklady earth sciences 2019-06, Vol.486 (2), p.711-715
Main Authors: Butvina, V. G., Vorobey, S. S., Safonov, O. G., Varlamov, D. A., Bondarenko, G. V., Shapovalov, Yu. B.
Format: Article
Language:English
Subjects:
Bearing
Carbonates
Chromite
Chromium
Crystallization
Earth and Environmental Science
Earth mantle
Earth Sciences
Garnet
Geochemistry
Ilmenite
Inclusions
Magma
Massifs
Minerals
Peridotite
Potassium
Rutile
Silicates
Titanates
Upper mantle
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Summary:The results of experiments on the synthesis of exotic titanates (priderite and yimengite) simulating metasomatic conditions of alteration of the mantle minerals (chromite and ilmenite) are reported. Ba-free Cr-bearing priderite was synthesized for the first time. Experiments showed the possibility of crystallization of this mineral as a product of the reaction of high-Cr spinel and rutile with hydrous–carbonate fluid (melt) under the conditions of the upper mantle. In particular, the experimental data obtained provide an interpretation of the relationships between K‒Cr priderite and carbonate–silicate inclusions in chromites from garnet peridotite of the Bohemian massif. Experimental study of the reaction of chromite and ilmenite with potassic hydrous–carbonate fluid (melt) shows the presence of both titanate phases (priderite and yimengite), the mineral indicators of mantle metasomatism. This provides direct evidence for the formation of yimengite and K‒Cr priderite, as well as other titanates, due to mantle metasomatism of the upper mantle peridotite under the conditions of the highest activities of potassium.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X19060254