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- W2086984328 abstract "The Podlesigranite stock (Czech Republic) is a fractionated, peraluminous, F-, Li- and P-rich, and Sn, W, Nb, Ta-bearing rare-metal granite system. Its magmatic evolution involved processes typical of intrusions related to porphyry type deposits (explosive breccia, comb layers), rare-metal granites (stockscheider), and rare metal pegmatites (extreme F-P-Li enrichment, Nb-Ta-Sn minerals, layering). Geological, textural and mineralogical data suggest that the Podlesigranites evolved from fractionated granitic melt progressively enriched in H2O, F, P, Li, etc. Quartz, K-feldspar, Fe-Li mica and topaz bear evidence of multistage crystallization that alternated with episodes of resorption. Changes in chemical composition between individual crystal zones and/or populations provide evidence of chemical evolution of the melt. Variations in rock textures mirror changes in the pressure and temperature conditions of crystallization. Equilibrium crystallization was interrupted several times by opening of the system and the consequent adiabatic decrease of pressure and temperature resulted in episodes of nonequilibrium crystallization. The Podlesigranites demonstrate that adiabatic fluctuation of pressure (bswinging eutecticQ) and boundary-layer crystallization of undercooled melt can explain magmatic layering and unidirectional solidification textures (USTs) in highly fractionated granites. D 2004 Elsevier B.V. All rights reserved." @default.
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- W2086984328 date "2005-03-01" @default.
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- W2086984328 title "Textural and chemical evolution of a fractionated granitic system: the Podlesí stock, Czech Republic" @default.
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- W2086984328 doi "https://doi.org/10.1016/j.lithos.2003.11.004" @default.
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