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P-T data of Ky-St-Grt gneisses hosting HP amphibolites and eclogites from the Austroalpine Polinik complex, Kreuzeck Mountains, Eastern Alps, Austria
Authors:Martin Michálek  Marián Puti?  Christoph A Hauzenberger
Institution:1. Department of Mineralogy and Petrology, Faculty of Natural Sciences, Comenius University, Mlynská dolina, 845 15, Bratislava, Slovakia
2. Department of Earth Sciences, Karl-Franzens-University Graz, Universit?tplatz 2, 8010, Graz, Austria
Abstract:This study focuses on metapelites of the Polinik complex in the Kreuzeck Mts. southeast of the Tauern Window, Eastern Alps, where kyanite — staurolite — garnet gneisses host eclogites and high pressure (HP) amphibolites of the Austroalpine basement. The stable mineral assemblage is garnet — staurolite — biotite — kyanite — quartz. Estimated metamorphic conditions from conventional geothermobarometry are 654±30 °C and 0.9±0.08 GPa, and Average P-T values calculated by THERMOCALC, are 665±15 °C at 0.77±0.09 GPa. Formation of the present mineral association in gneisses is related to the exhumation (D2) stage of hosted eclogites/HP amphibolites within a lateral strike-slip zone.
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