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- W2183632809 abstract "The northernmost Southalpine basement rocks, the Brixen quartzphyllites, which lack a Permian contact metamorphic overprint, were sampled near Waidbruck/Ponte Gardena and Spiluck/Spelonca in South-Tyrol, Italy. These samples contain the mineral assemblage muscovite + chlorite + albite + biotite + garnet + quartz ± K-feldspar. This mineral assemblage represents the Variscan peak metamorphic assemblage of the Southalpine basement and yields maximum P-T conditions of 0.53‐0.59 GPa and 521‐551°C using multi-equilibrium calculation thermobarometry using the software THERMOCALC v.3.23. Pseudosection modelling using the software THERIAK‐DOMINO was done using XRF bulk rock analyses of the samples. The obtained P-T data using the multi-equilibrium approach are slightly higher but still in very good agreement with the Variscan peak metamorphic conditions (T = 450‐550°C, P = 0.5‐0.65 GPa) estimated by RING & RICHTER (1994) using garnet-biotite thermometry and plagioclase‐biotite‐ garnet‐ muscovite barometry. In addition, the results of pseudosection modelling also agree very well with the observed mineral assemblages in the samples." @default.
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- W2183632809 date "2010-01-01" @default.
- W2183632809 modified "2023-09-28" @default.
- W2183632809 title "MULTI-EQUILIBRIUM- AND PSEUDOSECTION MODELLING OF THE NORTHERNMOST SOUTHALPINE BASEMENT (BRIXEN QUARTZPHYLLITE, SOUTH-TYROL, ITALY)" @default.
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