Registros del 1 al 10 de 19 encontrados |
![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 4.- Chronostratigraphy and tectonic deformation of the north Ecuadorian-south Colombian offshore Manglares forearc basin
Elsevier; Amsterdam; NLD; Netherlands, 2008
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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