National University of Salta, Argentina
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Affiliated Works
sorted by decreasing year, and then by display-name
- Late Quaternary Sedimentation and Erosion Rates Derived From Luminescence and Cosmogenic Nuclide Dating of Intermontane Basin Sediments, NW Argentine Cordillera
- SO<SUB>2</SUB> loss rates at Lascar volcano, Chile: preliminary results and interpretations from 2002 measurements
- Orogen-parallel Contraction in the Central Andes: Changing Plate Kinematics or Intrinsic Causes?
- Columnar jointing in non-welded Cerro Galan ignimbrite: Paycuqui, Argentina
- A global database of volcano edifice morphometry using SRTM DEMs
- Evolution of the Altiplano-Puna Margin in the Central Andes - Construction and Erosion (Invited)
- A previously unrecognised major orogenic front in Argentina
- Neogene-Quaternary Tectonics, Sedimentation, and Erosion of the Quebrada de Humahuaca and Casa Grande Basin, Intermontane Basins on the Margin of the Puna Plateau (23-24°S), NW Argentina
- Controls on Sediment Accumulation in Pliocene-Quaternary Intermontane Basins on the Margin of the Puna Plateau (23-24°S), NW Argentina
- Reconstructing the Mio-Pliocene South American Monsoon and Orographic Barrier Evolution (Angastaco Basin, NW Argentina)
- Multi-proxy reconstruction of the paleo-hydrological cycle during Andean Plateau uplift, NW-Argentina
- Orographic barrier development along the eastern flanks of the southern central Andes, Argentina: new insights from stable hydrogen isotopes in hydrated volcanic glass
- Potential Feedbacks Between Tectonics, Climate, and Sediment Accumulation in a Neogene-Quaternary Intermontane Basin on the Margin of the Puna Plateau, Quebrada de Humahuaca, NW Argentina
- Ages and potential drivers of fluvial fill terrace formation in the southern-central Andes, NW Argentina
- Genesis and Eruptive Dynamics of the Garnet-Bearing Rhyolites from the Ramadas Volcanic Centre (Altiplano-Puna Plateau, Central Andes, Argentina).
- Hydrogen stable isotopes from hydrated volcanic glass record orogenic growth and climate change at the eastern Puna Plateau margin, NW Argentina
- Landscape response to late Pleistocene climate change along the Puna Plateau margin: Sediment flux and cosmogenic landslide signatures modulated by basin geometry
- Linking hydrologic and bedload transport models to simulate fluvial response to changing precipitation
- Miocene to present-day shortening and intermontane basin formation in the Andean Puna Plateau, NW Argentina (24°30'S)
- Tectonics, climate, and landscape evolution of the southern-central Andes revealed by leaf wax stable isotopes
- Changes in denudation rates and erosion processes in the transition from a low-relief, arid orogen interior to a high-relief, humid mountain-front setting, Toro Basin, southern Central Andes
- Leaf-wax lipid biomarker paleoaltimetry and hydrologic evolution of the south-central Andean Plateau (Puna)