Experimental Study of the Formation of Chromium-Bearing Priderite and Yimengite as Products of Modal Mantle Metasomatism
Autor: | G. V. Bondarenko, Oleg G. Safonov, Yu. B. Shapovalov, S. S. Vorobey, V. G. Butvina, Dmitry A. Varlamov |
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Rok vydání: | 2019 |
Předmět: |
Peridotite
geography geography.geographical_feature_category Mineral 010504 meteorology & atmospheric sciences Spinel Geochemistry Massif engineering.material 010502 geochemistry & geophysics 01 natural sciences Rutile Earth and Planetary Sciences (miscellaneous) engineering General Earth and Planetary Sciences Chromite Metasomatism Ilmenite Geology 0105 earth and related environmental sciences |
Zdroj: | Doklady Earth Sciences. 486:711-715 |
ISSN: | 1531-8354 1028-334X |
DOI: | 10.1134/s1028334x19060254 |
Popis: | 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. |
Databáze: | OpenAIRE |
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