Registros del 1 al 10 de 19 encontrados |
1.- About the nature of a seismic barrier and a seismic asperity; evidence from seismic data collected across rupture zones of great Ecuador-Colombia subduction earthquakes [International Geological Congress]; [location varies]; III; International, 2004 Italia 2004; 32nd international geological congress; abstracts Ver registro
2.- An overview of the submarine morphology of the Ecuador-south Colombia convergent margin; implication for mass transfer and age of the Carnegie Ridge subduction Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010 European Geosciences Union general assembly 2010 Ver registro
3.- ARE RUPTURE ZONE LIMITS OF GREAT SUBDUCTION EARTHQUAKES CONTROLLED BY UPPER PLATE STRUCTURES? EVIDENCE FROM MULTICHANNEL SEISMIC REFLECTION DATA ACQUIRED ACROSS THE NORTHERN ECUADOR; SOUTHWEST COLOMBIA MARGIN AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004 Ver registro
4.- Chronostratigraphy and tectonic deformation of the north Ecuadorian-south Colombian offshore Manglares forearc basin Elsevier; Amsterdam; NLD; Netherlands, 2008 Ver registro
5.- Crustal structure and tectonic deformation of the southern Ecuadorian margin Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010 European Geosciences Union general assembly 2010 Ver registro
6.- DEEP STRUCTURES OF THE ECUADOR CONVERGENT MARGIN AND THE CARNEGIE RIDGE, POSSIBLE CONSEQUENCE ON GREAT EARTHQUAKES RECURRENCE INTERVAL AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004 Ver registro
7.- FIELDS OF MULTI-KILOMETER SCALE SUB-CIRCULAR DEPRESSIONS IN THE CARNEGIE RIDGE SEDIMENTARY BLANKET; EFFECT OF UNDERWATER CARBONATE DISSOLUTION? ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2005 Ver registro
8.- In north Ecuador-south Colombia margin (0-4 degrees N), the sedimentation rate in the trench and the tectonic deformation co-control the location of the seismogenic zone Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010 European Geosciences Union general assembly 2010 Ver registro
9.- Late Quaternary geomorphologic evolution of submarine canyons as a marker of active deformation on convergent margins; the example of the south Colombian margin Elsevier; Amsterdam; NLD; Netherlands, 2012 Ver registro
10.- Mass-transport deposits in the northern Ecuador subduction trench; result from frontal erosion over multiple seismic cycles Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010 European Geosciences Union general assembly 2010 Ver registro
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