Alpine regional metamorphism of Föderata Group metacarbonates (southern Veporicum, Western Carpathians, Slovakia): P–T conditions of recrystallization

• Autorzy: Ružička P. , Vozárová A. , Michálek M. , Dyda M.
• Języki publikacji: EN

Abstrakty

EN

P-T conditions of the Alpine regional metamorphism of carbonate successions which form the cover sequence of the southern Veporicum crystalline basement have been determined. The P-T estimates were calculated on the basis of microprobe chemical analyses of equilibrium mineral assemblages together with analyses of bulk rock chemical composition. The calibrated geothermic reactions Cal-Dol and Kfs-Phl were used. Geothermometric and geobarometric data were obtained using the SOLVCALC, TWQ and PERPLEX software programs in combination with phengite geobarometry. The metacarbonates were formed from a sedimentary-carbonate protolith in low-pressure and low-temperature conditions of greenschist facies in the kyanite stability field: T_CalAb-Or

Słowa kluczowe

EN

south ern Veporicum; geothermobarometry; metacarbonates; Alpine metamorphism

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2011
• Tom: Vol. 55, No. 1
• Strony: 9--26
• Opis fizyczny: Bibliogr. 50 poz., rys., tab., wykr.

Twórcy

autor

Ružička P.

autor

Vozárová A.

autor

Michálek M.

autor

Dyda M.

• Faculty of Natural Sciences, Comenius University, Department Mineralogy and Petrology, Mlynská dolina G, 84215 Bratislava, Slovakia,

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