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

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 upper-cr...

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Detalles Bibliográficos
Autores principales: Herwegh, Marco, Berger, Alfons, Baumberger, Roland, Wehrens, Philip, Kissling, Edi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5428471/
https://www.ncbi.nlm.nih.gov/pubmed/28341833
http://dx.doi.org/10.1038/s41598-017-00440-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5428471/
https://www.ncbi.nlm.nih.gov/pubmed/28341833
http://dx.doi.org/10.1038/s41598-017-00440-0

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