| Registros del 1 al 10 de 13 encontrados |
1.- About the relationship between forearc anatomy and megathrust earthquakes
American Geophysical Union; Washington, DC; USA; United States, 2006
AGU 2006 fall meeting
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2.- Active faulting, surface deformation and subduction earthquakes at Isla Santa Maria, south-central Chile
American Geophysical Union; Washington, DC; USA; United States, 2004
AGU 2004 fall meeting
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3.- DEVELOPMENT OF A LANDSLIDE HAZARD MAP FOR NORTHWEST ARGENTINA
EUROPEAN GEOPHYSICAL SOCIETY; KATHLENBURG-LINDAU; DEU; FEDERAL REPUBLIC OF GERMANY, 1998
23RD GENERAL ASSEMBLY OF THE EUROPEAN GEOPHYSICAL SOCIETY; PART 1, SOCIETY SYMPOSIA, SOLID EARTH, GEOPHYSICS AND GEODESY
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4.- Does the topographic distribution of the central Andean Puna Plateau result from climatic or geodynamic processes?
Geological Society of America (GSA); Boulder, CO; USA; United States, 2009
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5.- Neogene to Quaternary broken foreland formation and sedimentation dynamics in the Andes of NW Argentina (25 degrees S)
American Geophysical Union; Washington, DC; USA; United States, 2011
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6.- Orographic barriers, high-resolution TRMM rainfall, and relief variations along the eastern Andes
American Geophysical Union; Washington, DC; USA; United States, 2007
AGU 2007 fall meeting
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7.- Precipitation, focused erosion and crustal flexural accommodation in the eastern Altiplano (Bolivia)
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008
European Geosciences Union general assembly 2008
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8.- Quaternary tectonic tilting governed by rupture segments controls surface morphology and drainage evolution along the south-central coast of Chile
American Geophysical Union; Washington, DC; USA; United States, 2004
AGU 2004 fall meeting
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9.- Tectonics and climate of the southern Central Andes
Annual Reviews; Palo Alto, CA; USA; United States, 2007
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10.- The topographic imprint of a transient climate episode; the western Andean flank between 15.5 degrees and 41.5 degrees S
Wiley; Chichester; GBR; United Kingdom, 2010
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