Browsing by Author "Farías, M."

Now showing items 1-3 of 3

    • Differences in Be-10 concentrations between river sand, gravel and pebbles along the western side of the ... 
      Carretier, S.; Regard, V.; Vassallo, R.; Aguilar, G.; Martinod, J.; Riquelme, R.; Christophoul, F.; Charrier González, Reynaldo; Gayer, E.; Farías, M.; Audin, L.; Lagane, C. (Elsevier, 2015)
      Cosmogenic nuclides in river sediment have been used to quantify catchment-mean erosion rates. Nevertheless, variable differences in Be-10 concentrations according to grain size have been reported. We analyzed these ...
    • Pleistocene landscape entrenchment: a geomorphological mountain to foreland field case, the LasTunas system, ... 
      Pepin, E.; Carretier, Sébastien; Hérail, G.; Regard, V.; Charrier González, Reynaldo; Farías, M.; García, V.; Giambiagi, L. (Basin Research, John Wiley & Sons, 2013)
      The study of the Las Tunas River incisions, located in the eastern Andean foreland front (33 20’ S in Argentina), provides new clues for the interpretation of deep piedmont entrenchments. Both the Las Tunas mountain ...
    • Slope and climate variability control of erosion in the Andes of central Chile 
      Carretier, Sébastien; Regard, V.; Vassallo, R.; Aguilar, G.; Martinod, J.; Riquelme Vásquez, René; Pepin, E.; Charrier González, Reynaldo; Hérail, G.; Farías, M.; Guyot, J. L.; Vargas, G.; Lagane, C. (2013)
      Climate and topography control millennial-scale mountain erosion, but their relative impacts remain matters of debate. Confl icting results may be explained by the infl uence of the erosion threshold and daily variability ...