Инд. авторы:	Chepurov A.A., Faryad S.W., Agashev A.M., Strnad L., Jedlicka R., Turkin A.I., Mihaljevic M., Lin V.V.
Заглавие:	Experimental crystallization of a subcalcic Cr-rich pyrope in the presence of REE-bearing carbonatite
Библ. ссылка:	Chepurov A.A., Faryad S.W., Agashev A.M., Strnad L., Jedlicka R., Turkin A.I., Mihaljevic M., Lin V.V. Experimental crystallization of a subcalcic Cr-rich pyrope in the presence of REE-bearing carbonatite // Chemical Geology. - 2019. - Vol.509. - P.103-114. - ISSN 0009-2541. - EISSN 1878-5999.
Идентиф-ры:	DOI: 10.1016/j.chemgeo.2019.01.011; РИНЦ: 38668055; SCOPUS: 2-s2.0-85061117092; WoS: 000459780600007;
Реферат:	eng: This paper focuses on formation of subcalcic Cr-rich garnet (up to 14.25 wt% Cr2O3) in the model ultramafic system corresponding to natural harzburgite with the presence of REE-bearing fluid phase. The experiments were carried out using a "split-sphere" type multi-anvil high-pressure apparatus (BARS) at a pressure of 5 GPa and a temperature of 1300 degrees C. Natural serpentine, chromite, corundum and REE-carbonatite were used as starting components. Crystallization of garnet occurred in subsolidus conditions by the reaction of orthopyroxene and spinel in the presence of fluid phase. Composition of fluid was controlled by interaction of water released by decomposition of serpentine with carbonate. By using different amounts of carbonatite (0.5 and 1.5 wt%) as a source of calcium and REE, subcalcic Cr-rich garnets with up to 3.5 wt% CaO were crystallized, which are typical for inclusions of harzburgitic paragenesis in natural diamonds. The experiments demonstrated that the rare earth elements (REE) released from the initial carbonatite were transported by the fluid and were incorporated into the newly formed garnet. The distribution of REE in garnet revealed a vivid enrichment toward the heavy REE (HREE), showing the pattern with a very steep slope. These results confirmed high partitioning of HREE into garnet. The present study indicates that the mantle carbonatites, which contain very high proportions of light REE (LREE) to HREE, can play an important role as source material in formation of REE-rich fluids to crystallize garnets with typical REE patterns in mantle peridotites.
Ключевые слова:	DYKE SYSTEM; HIGH-PRESSURE; GARNET XENOCRYSTS; MINERAL INCLUSIONS; PERIDOTITE XENOLITHS; METASOMATIC PROCESSES; LITHOSPHERIC MANTLE; GRIB KIMBERLITE PIPE; SLAB MANTLE INTERACTIONS; Experimental petrology; High pressure; Diamond; Carbonatite; Rare earth elements; Serpentinite; Subcalcic garnet; DIAMONDS;
Издано:	2019
Физ. хар-ка:	с.103-114