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Rapid surface uplift and crustal flow in the Central Andes (southern Peru) controlled by lithospheric drip dynamics

The high flux magmatism, crustal shortening/extension and plateau formation in Cordilleran orogenic systems have been explained by removal of lithosphere (lower crust and the sub-arc mantle lithosphere) that develops beneath the magmatic arc and hinterland regions. However, the primary role of this...

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Detalles Bibliográficos
Autores principales: Göğüş, Oğuz H., Sundell, Kurt, Uluocak, Ebru Şengül, Saylor, Joel, Çetiner, Uğurcan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8975996/
https://www.ncbi.nlm.nih.gov/pubmed/35365670
http://dx.doi.org/10.1038/s41598-022-08629-8