REE Minerals as Geochemical Proxies of Late-Tertiary Alkalic Silicate ± Carbonatite Intrusions Beneath Carpathian Back-Arc Basin

نویسندگان

چکیده

The accessory mineral assemblage (AMA) of igneous cumulate xenoliths in volcanoclastic deposits and lava flows the Carpathian back-arc basin testifies to composition intrusive complexes sampled by Upper Miocene-Pliocene basalt volcanoes. magmatic reservoir beneath Pinciná maar is composed gabbro, moderately alkalic alkali-calcic syenite, calcic orthopyroxene granite (pincinite). complex wider area around Fi?akovo Hajná?ka maars contains mafic cumulates, carbonatite, calc-alkalic granite. Both reservoirs originated during basaltic magma underplating, differentiation, interaction with surrounding mantle crust. AMA syenites characterized yttrialite-Y, britholite-Y, britholite-Ce, chevkinite-Ce, monazite-Ce, rhabdophane(?). Baddeleyite REE-zirconolite are typical syenite associated carbonatite. Pyrochlore, columbite-Mn, Ca-niobates occur granites strong peralkalic affinity. Nb-rutile, niobian ilmenite, fergusonite-Y crystallized from mildly Zircons increased Hf/Zr Th/U ratios all felsic-to-intermediate rock-types. If rock fragments absent volcanic ejecta, sub-volcanic can be reconstructed specific zircon xenocrysts–xenolith relics disintegrated fragmentation explosion.

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ژورنال

عنوان ژورنال: Minerals

سال: 2021

ISSN: ['2075-163X']

DOI: https://doi.org/10.3390/min11040369