Registros del 1 al 10 de 11 encontrados |
1.- 3D SEISMIC REFRACTION TOMOGRAPHY OF OCEAN BOTTOM HYDROPHONE DATA RECORDED OFFSHORE VALPARAISO, CHILE EUROPEAN GEOPHYSICAL SOCIETY; KATHLENBURG-LINDAU; DEU; FEDERAL REPUBLIC OF GERMANY, 1998 23RD GENERAL ASSEMBLY OF THE EUROPEAN GEOPHYSICAL SOCIETY; PART I, SOCIETY SYMPOSIA, SOLID EARTH GEOPHYSICS AND GEODESY Ver registro
2.- CRUSTAL STRUCTURE IN SOUTHERN COSTA RICA FROM SEISMIC WIDE-ANGLE EXPERIMENTS AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1996 AGU 1996 FALL MEETING Ver registro
3.- Intraplate seismicity and mantle hydration at the Nicaraguan Trench outer rise American Geophysical Union; Washington, DC; USA; United States, 2008 AGU 2008 fall meeting Ver registro
4.- LOCAL EARTHQUAKE TOMOGRAPHY IN THE ANTOFAGASTA (CHILE) REGION AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1999 AGU 1999 FALL MEETING Ver registro
5.- Margin architecture and seismic attenuation in the central Costa Rican forearc Elsevier; Amsterdam; NLD; Netherlands, 2010 Ver registro
6.- SEISMIC INVESTIGATIONS OFFSHORE NICARAGUA AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1996 AGU 1996 FALL MEETING Ver registro
7.- Seismic structure of the Nicaragua convergent margin by travel time tomographic inversion of wide-angle seismic data Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2009 European Geosciences Union general assembly 2009 Ver registro
8.- Seismicity in the outer rise offshore southern Chile; indication of fluid effects in crust and mantle Elsevier; Amsterdam; NLD; Netherlands, 2008 Ver registro
9.- SEISMOGENIC PLANE OF THE NORTHERN ANDEAN SUBDUCTION ZONE FROM AFTERSHOCKS OF THE ANTOFAGASTA (CHILE) 1995 EARTHQUAKE AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002 Ver registro
10.- STRUCTURE AND TECTONICS OF THE EROSIONAL CONVERGENT MARGIN OFF ANTOFAGASTA, NORTH CHILE (23 DEGREES 30'S) AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2005 Ver registro
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