Large-Scale Crustal-Block-Extrusion During Late Alpine Collision

Abstract The crustal-scale geometry of the European Alps has been explained by a classical subduction-scenario comprising thrust-and-fold-related compressional wedge tectonics and isostatic rebound. However, massive blocks of crystalline basement (External Crystalline Massifs) vertically disrupt the...

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Autores principales: Marco Herwegh, Alfons Berger, Roland Baumberger, Philip Wehrens, Edi Kissling
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/a0dfb31a2f0841e3a64f5f43a90182f3
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