Origin of andradite in the Quaternary volcanic Andahua Group, Central Volcanic Zone, Peruvian Andes

نویسندگان

چکیده

Abstract Euhedral andradite crystals were found in trachyandesitic (latitic) lavas of the volcanic Andahua Group (AG) Central Andes. The AG comprises around 150 centers, most wich are monogenetic. studied is complexly zoned (enriched Ca and Al its core mantle, Fe this compositionally homogenous rim). core-mantle regions contain inclusions anhydrite, halite, S- Cl-bearing silicate glass, quartz, anorthite, wollastonite magnetite clinopyroxene. chemical compositions garnet suggest their contact metamorphic to pyrometamorphic origin. observed zoning pattern changes type abundance indicative an abrupt change temperature subsequent devolatilization sulfates halides during growth. This process interpreted have taken place entirely within a captured xenolith evaporite-bearing wall rock host magma. devolitilization sediments, especially sulfur-bearing phases, may resulted occasional but voluminous emissions gases be regarded as potential hazard associated with volcanism.

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ژورنال

عنوان ژورنال: Mineralogy and Petrology

سال: 2021

ISSN: ['1438-1168', '0930-0708']

DOI: https://doi.org/10.1007/s00710-021-00744-0