Crustal attenuation in the Southern Andean retroarc (38°-39°30′ S) determined from tectonic and gravimetric studies: The Lonco-Luán asthenospheric anomaly
The western retroarc of the Southern Andes between 38° and 40° S is formed by a NNW-elongated ridge not associated with stacked thrust sheets. On the contrary, during the last 4-3 Ma this ridge was affected by extensional deformation, regional uplift and related folding on a very broad scale. Receiv...
Guardado en:
| Autores principales: | Folguera, Andrés, Tunstall, Cynthia, Garcia Morabito, Ezequiel, Ramos, Victor Alberto |
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| Publicado: |
2007
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| Materias: | |
| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00401951_v439_n1-4_p129_Folguera http://hdl.handle.net/20.500.12110/paper_00401951_v439_n1-4_p129_Folguera |
| Aporte de: |
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