Episyenites in meta-granitoids of the Tauern Window (Eastern Alps): unpredictable?

Autor: Giorgio Pennacchioni, Claudio Mazzoli, Patrizia Ferretti, Alberto Ceccato, Federico Zorzi, A. M. Fioretti

Publikováno v: Journal of geodynamics 101 (2016): 73–87. doi:10.1016/j.jog.2016.04.001
info:cnr-pdr/source/autori:Pennacchioni G.[1], Ceccato A.[1], Fioretti A.M.[2], Mazzoli C.[1], Zorzi F.[1], Ferretti P.[3]/titolo:Episyenites in meta-granitoids of the Tauern Window (Eastern Alps): unpredictable?/doi:10.1016%2Fj.jog.2016.04.001/rivista:Journal of geodynamics/anno:2016/pagina_da:73/pagina_a:87/intervallo_pagine:73–87/volume:101

The core of the Tauern tectonic window (Eastern Alps) consists of pre-Alpine granitoids (∼295 Ma) variably deformed during Alpine (∼30Ma) amphibolite-facies metamorphism. Episyenites occur as local alteration haloes (as wide as a few meters) surr

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http://hdl.handle.net/11585/757885