Instituto Geológico y Minero de España

LogoSistema de información documental - SID

 

 

 

Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 7 de 7 encontrados

1.-  From ductile to brittle, late- to post-orogenic evolution of the Betic Cordillera; structural insights from the northeastern Internal zones
Societe Geologique de France; Paris; FRA; France, 2013
Ver registro

2.-  PRESSURE-TEMPERATURE-TIME CONSTRAINTS ON THE MAGHREBIDE MOUNTAIN BUILDING; EVIDENCE FROM THE RIF-BETIC TRANSECT (MOROCCO, SPAIN), ALGERIAN CORRELATIONS, AND GEODYNAMIC IMPLICATIONS
ELSEVIER; PARIS; FRA; FRANCE, 2006
QUELQUES DEVELOPPEMENTS RECENTS SUR LA GEODYNAMIQUE DU MAGHREB--SOME RECENT DEVELOPMENTS ON THE MAGHREB GEODYNAMICS
Ver registro

3.-  Subduction, convergence and the mode of backarc extension in the Mediterranean region
Societe Geologique de France; Paris; FRA; France, 2008
Ver registro

4.-  The Atlas Mountains; Why there? Why now?
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
Ver registro

5.-  The building of the Betic-Rif Orogen and the geodynamic evolution of western Mediterranean
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2009
European Geosciences Union general assembly 2009
Ver registro

6.-  The building of the Betic-Rif orogen and the geodynamics of western Mediterranean; constraints from the tectonic and metamorphic evolution of the Alboran Domain and the External Rif
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
Ver registro

7.-  Thermal structure of the Sebtide and Ghomaride nappes in the Rif Belt (northern Morocco); correlations with Alpujarride and Malaguide complexes in western Betics; SE Spain
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
Ver registro


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