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 |
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Přispěvatelé: | Pennacchioni G., Ceccato A., Fioretti A.M., Mazzoli C., Zorzi F., Ferretti P. |
Jazyk: | angličtina |
Rok vydání: | 2016 |
Předmět: |
010504 meteorology & atmospheric sciences
Tauern tectonic window Settore GEO/03 - Geologia Strutturale δ Geochemistry Metamorphism Episyenite 010502 geochemistry & geophysics 01 natural sciences Cataclastic fault Meta-granitoid Cataclastic faults Fluid-rock interaction Meta-granitoids δ18O isotopes Earth-Surface Processes Geophysics Geomorphology 0105 earth and related environmental sciences O isotopes Cataclastic faults Episyenite Fluid-rock interaction Meta-granitoids Tauern tectonic window δ18O isotopes Earth-Surface Processes Geophysics Tectonics Settore GEO/08 - Geochimica e Vulcanologia Delta18 isotopes Geology |
Zdroj: | 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 |
DOI: | 10.1016/j.jog.2016.04.001 |
Popis: | 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) surrounding steeply dipping, strike-slip faults, with offsets |
Databáze: | OpenAIRE |
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