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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...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2022
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| 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 |