Registros del 1 al 10 de 14 encontrados |
![](./images/clear.gif) 1.- 2D fine-scale imaging of the subduction channel in Gulf of Guayaquil by integrated iterative PSDM and simulated annealing optimization
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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![](./images/clear.gif) 2.- EXPLORING THE ECUADOR-COLUMBIA ACTIVE MARGIN AND INTERPLATE SEISMOGENIC ZONE
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
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![](./images/clear.gif) 3.- Interplate patchiness and subduction-erosion mechanisms; evidence from depth-migrated seismic images at the central Ecuador convergent margin
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
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![](./images/clear.gif) 4.- Joint inversion of multichannel seismic reflection and wide-angle seismic data; improved imaging and refined velocity model of the crustal structure of the north Ecuador-south Colombia convergent margin
American Geophysical Union; Washington, DC; USA; United States, 2009
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![](./images/clear.gif) 5.- Joint ray + Born least-squares migration and simulated annealing optimization for target-oriented quantitative seismic imaging
Society of Exploration Geophysicists; Tulsa, OK; USA; United States, 2011
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![](./images/clear.gif) 6.- Morphotectonic variations along the north Ecuador-south Colombia margin (1-4 degrees N); control on the location of the thermally-defined seismogenic zone
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008
European Geoscience Union general assembly 2008
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![](./images/clear.gif) 7.- Origin of a crustal splay fault and its relation to the seismogenic zone and underplating at the erosional north Ecuador-south Colombia oceanic margin
American Geophysical Union; Washington, DC; USA; United States, 2008
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![](./images/clear.gif) 8.- Plio-Quaternary uplift of the Manta Peninsula and La Plata Island and the subduction of the Carnegie Ridge, central coast of Ecuador
Elsevier; Oxford; GBR; United Kingdom, 2006
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![](./images/clear.gif) 9.- Prominent influence of trench sedimentation rate on heat flow and location of the thermally-defined seismogenic zone in convergent margin; example of the north Ecuador-south Colombia margin (1-4 degrees N)
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008
European Geoscience Union general assembly 2008
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![](./images/clear.gif) 10.- SEAFLOOR MARGIN MAP HELPS IN UNDERSTANDING SUBDUCTION EARTHQUAKES
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2005
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