Permian-Triassic high thermal regime in the Alps: result of Late Variscan collapse or continental rifting? Validation by numerical modeling

Autor: Marotta A.M., Spalla M.I.

Publikováno v: Tectonics (Washington, D.C.) 26 (2007): 1–27. doi:10.1029/2006TC002047
info:cnr-pdr/source/autori:Marotta A.M., Spalla M.I./titolo:Permian-Triassic high thermal regime in the Alps: result of Late Variscan collapse or continental rifting? Validation by numerical modeling./doi:10.1029%2F2006TC002047/rivista:Tectonics (Washington, D.C.)/anno:2007/pagina_da:1/pagina_a:27/intervallo_pagine:1–27/volume:26

The Permian-Triassic igneous activity, associated with regional scale deformation developed under high-temperature/low-pressure (HT-LP) metamorphic conditions and widely recorded in the pre-Alpine crust of the European Alps, can result from late orog

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https://publications.cnr.it/doc/20179

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