Registros del 1 al 9 de 9 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.- 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) 6.- Structure of the Malpelo Ridge (Colombia) from seismic and gravity modelling
Springer; Dordrecht; NLD; Netherlands, 2006
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![](./images/clear.gif) 7.- The 2010 Haiti earthquake; a complex fault pattern constrained by seismologic and tectonic observations
American Geophysical Union; Washington, DC; USA; United States, 2011
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![](./images/clear.gif) 8.- Thermal regime from bottom simulating reflectors along the north Ecuador-south Colombia margin; relation to margin segmentation and great subduction earthquakes
American Geophysical Union; Washington, DC; USA; United States, 2006
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![](./images/clear.gif) 9.- Thermal segmentation along the N. Ecuador-S. Colombia margin (1-4 degrees N); prominent influence of sedimentation rate in the trench
Elsevier; Amsterdam; NLD; Netherlands, 2008
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