作者: Anna Vozárová , Marian Dyda , Martin Michálek , Peter Ružička
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摘要: P-T conditions of the Alpine regional metamorphism carbonate successions which form cover sequence southern Veporicum crystalline basement have been determined. The estimates were calculated on basis microprobe chemical analyses equilibrium mineral assemblages together with bulk rock composition. calibrated geothermic reactions Cal-Dol and Kfs-Phl used. Geothermometric geobarometric data obtained using SOLVCALC, TWQ PERPLEX software programs in combination phengite geobarometry. metacarbonates formed from a sedimentary-carbonate protolith low-pressure low-temperature greenschist facies kyanite stability field: TCal = 354-476°C, TAb-Or 329-453°C, P 0.3-0.5 GPa, during Cretaceous orogeny