Registros del 1 al 10 de 12 encontrados |
![](./images/clear.gif) 1.- Crustal seismicity and 3-D velocity structure in the principal Cordillera of central Chile (33-34.5 S, 69.5-71 W); implications on Andean geodynamic and seismic hazard
American Geophysical Union; Washington, DC; USA; United States, 2007
AGU 2007 fall meeting
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![](./images/clear.gif) 2.- CRUSTAL STRUCTURE OF THE SOUTHERNMOST CHILEAN MARGIN FROM SEISMIC AND GRAVITY DATA
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2000
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![](./images/clear.gif) 3.- FLAT-SLAB TO STEEP SUBDUCTION TRANSITION ZONE IN CENTRAL CHILE-WESTERN ARGENTINA; BODY WAVES TOMOGRAPHY AND STATE OF STRESS
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004
AGU 2004 FALL MEETING
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![](./images/clear.gif) 4.- INVERSION OF AN OLIGOCENE VOLCANO-TECTONIC BASIN AND UPLIFTING OF ITS SUPERIMPOSED MIOCENE MAGMATIC ARC IN THE CHILEAN CENTRAL ANDES; FIRST SEISMIC AND GRAVITY EVIDENCES
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 1999
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![](./images/clear.gif) 5.- MANTLE FLOW THROUGH THE DRAKE PASSAGE; TELESEISMIC SHEAR WAVE SPLITTING RESULTS FROM THE SEPA EXPERIMENT
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1997
AGU 1997 FALL MEETING
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![](./images/clear.gif) 6.- MOCHA ISLAND IN SOUTH-CENTRAL CHILE; SOME CLUES ON A RAPID UPLIFTING HISTORY
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1994
AGU 1994 FALL MEETING
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![](./images/clear.gif) 7.- MODELIZACION DE LA ESTRUCTURA LITOSFERICA DEL MARGEN SUR CHILENO A PARTIR DE DATOS GRAVIMETRICOS Y SISMICOS
1996
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![](./images/clear.gif) 8.- Seismic analysis and distribution of a bottom-simulating reflector (BSR) in the Chilean margin offshore of Valdivia (40 degrees S)
Elsevier; Oxford; GBR; United Kingdom, 2009
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![](./images/clear.gif) 9.- STRUCTURAL VARIABILITY AT THE ACTIVE CONTINENTAL MARGIN OFF SOUTHERNMOST CHILE
PERGAMON PRESS; OXFORD - NEW YORK; III; INTERNATIONAL, 1999
LITHOSPHERIC STRUCTURE AND SEISMICITY AT CONVERGENT MARGINS
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![](./images/clear.gif) 10.- The flat subduction in central Chile-western Argentina (30-32 degrees S); a mineralogical interpretation based on P and S tomographic velocity models
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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