Registros del 1 al 10 de 13 encontrados |
![](./images/clear.gif) 1.- A morphotectonic analysis of central Patagonian Cordillera; negative inversion of the Andean belt over a buried spreading center?
American Geophysical Union; Washington, DC; USA; United States, 2010
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![](./images/clear.gif) 2.- 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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![](./images/clear.gif) 3.- Active faulting and heterogeneous deformation across a megathrust segment boundary from GPS data, south central Chile (36-39 degrees S)
American Geophysical Union and The Geochemical Society;; USA; United States, 2008
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![](./images/clear.gif) 4.- 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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![](./images/clear.gif) 5.- Glacial age accretion along the south-central Chile margin and inversion of forearc basins
American Geophysical Union; Washington, DC; USA; United States, 2006
AGU 2006 fall meeting
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![](./images/clear.gif) 6.- Heterogeneous plate locking in the south-central Chile subduction zone; building up the next great earthquake
Elsevier; Amsterdam; NLD; Netherlands, 2011
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![](./images/clear.gif) 7.- INVESTIGATING ACTIVE FAULTING IN THE SOUTH-CENTRAL CHILEAN FOREARC BY LOCAL SEISMICITY AND MOMENT TENSOR INVERSIONS
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004
AGU 2004 FALL MEETING
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![](./images/clear.gif) 8.- Neogene tectonic evolution of the Neuquen Andes western flank (37-39 degrees S)
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Evolution of an Andean margin; a tectonic and magmatic view from the Andes to the Neuquen Basin (35 degrees -39 degrees S lat)
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![](./images/clear.gif) 9.- PARTICION DE LA DEFORMACION EN LA ZONA DEL ARCO VOLCANICO DE LOS ANDES NEUQUINOS (36-39ºS) EN LOS ULTIMOS 30 MILLONES DE AÑOS
2002
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![](./images/clear.gif) 10.- 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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