Registros del 1 al 6 de 6 encontrados |
![](./images/clear.gif) 1.- A dynamic model of rifting between Galicia Bank and Flemish Cap during the opening of the North Atlantic Ocean
Geological Society of London; London; GBR; United Kingdom, 2007
Imaging, mapping and modelling continental lithosphere extension and breakup
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![](./images/clear.gif) 2.- Asymmetry and heterogeneity of crustal structure at magma-poor rifted margins; distribution of extension in space and time
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) 3.- CRUSTAL STRUCTURE OF THE OCEAN-CONTINENT TRANSITION AT FLEMISH CAP; SEISMIC REFRACTION RESULTS
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2003
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![](./images/clear.gif) 4.- Extension discrepancy at North Atlantic nonvolcanic rifted margins; depth-dependent stretching or unrecognized faulting?
Geological Society of America (GSA); Boulder, CO; USA; United States, 2007
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![](./images/clear.gif) 5.- Movement along a low-angle normal fault; the S reflector west of Spain
American Geophysical Union and The Geochemical Society;; USA; United States, 2007
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![](./images/clear.gif) 6.- THE DEEP STRUCTURE OF NON-VOLCANIC RIFTED CONTINENTAL MARGINS
ROYAL SOCIETY OF LONDON; LONDON; GBR; UNITED KINGDOM, 1999
RESPONSE OF THE EARTH'S LITHOSPHERE TO EXTENSION
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