Browsing by Subject "Patagonian Andes"

Now showing items 1-4 of 4

    • Evolution of surface characteristics of three debris-covered glaciers in the patagonian Andes from 1958 to 2020 
      Falaschi, Daniel; Rivera Ibáñez, Sergio Andrés; Lo Vecchio Repetto, Andrés; Moragues, Silvana; Villalba, Ricardo; Rastner, Philipp; Zeller, Josias; Salcedo, Ana Paula (Frontiers Media, 2021)
      A number of glaciological observations on debris-covered glaciers around the globe have shown a delayed length and mass adjustment in relation to climate variability, a behavior normally attributed to the ice insulation ...
    • Liquiñe‑Ofqui’s fast slipping intra‑volcanic arc crustal faulting above the subducted Chile Ridge 
      De Pascale, Gregory P.; Froude, Melanie; Penna, Ivanna; Hermanns, Reginald L; Sepúlveda, Sergio A.; Moncada, Daniel; Pérsico, Mario; Easton Vargas, Gabriel; Villalobos, Angelo; Gutiérrez, Francisco (Nature Research, 2021)
      The southernmost portion of the Liquiñe-Ofqui fault zone (LOFZ) lies within the proposed slab window which formed due to oblique subduction of the Chile Ridge in Patagonia. Mapping of paleo-surface ruptures, offsets, and ...
    • Retroarc deformation and exhumation near the end of the Andes, southern Patagonia 
      Fosdick, Julie C.; Grove, Marty; Hourigan, JeremyK.; Calderón, Mauricio (Elsevier, 2013)
      The southern Patagonian Andes constitute the narrow, high-latitude end of the Andean orogen belt in South America, where inherited basin paleogeography, subduction processes, retroarc crustal thickening, and late Cenozoic ...
    • The low-grade Canal de las Montañas Shear Zone and its role in the tectonic emplacement of the Sarmiento ... 
      Calderón, M.; Fosdick, J. C.; Warren, C.; Massonne, H. J.; Fanning, C. M.; Fadel Cury, L.; Schwanethal, J.; Fonseca, P. E.; Galaz, Gaspar; Gaytán, D.; Hervé Allamand, Francisco (Elsevier, 2012)
      The Canal de las Montañas Shear Zone (CMSZ), southern Patagonian Andes (51–52°S), is a low-grade mylonite belt generated from felsic ignimbritic, pelitic and basaltic protoliths of the Late Jurassic–Early Cretaceous Rocas ...