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![](./images/clear.gif) 1.- EARLY VARISCAN TECTONIC EVENTS IN VIANA DO ALENTEJO-ALVITO'S REGION, SW OSSA MORENA ZONE (SOUTHERN IBERIAN VARISCAN FOLD BELT)
CAMBRIDGE PUBLICATIONS; CAMBRIDGE; GBR; UNITED KINGDOM, 1999
EUROPEAN UNION OF GEOSCIENCES CONFERENCE ABSTRACTS; EUG 10
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![](./images/clear.gif) 2.- Seafloor morphology of the Eurasia-Nubia (Africa) plate boundary between the Tore-Madeira Rise and the Straits of Gibraltar; a case of coexistent Mesozoic through present day features of tectonic, oceanographic and sedimentary origin
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.- VIANA DO ALENTEJO-ALVITO'S ANTIFORM MACROSTRUCTURE (SW IBERIA-OSSO MORENA ZONE); EXPERIMENTAL MODELLING OF MULTILAYER SHEATH FOLD GENERATION BY HOMOGENEOUS SIMPLE SHEAR
CAMBRIDGE PUBLICATIONS; CAMBRIDGE; GBR; UNITED KINGDOM, 1999
EUROPEAN UNION OF GEOSCIENCES CONFERENCE ABSTRACTS; EUG 10
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