Instituto Geológico y Minero de España

LogoSistema de información documental - SID

 

 

 

Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 8 de 8 encontrados

1.-  Fault-related hydrothermal dolomites in Cretaceous carbonates (Cantabria, northern Spain); results of petrographic, geochemical and petrophysical studies
Societe Geologique de France; Paris; FRA; France, 2010
Hydrothermalisme en domaine continental ;Hydrothermalism in the continental domain
Ver registro

2.-  Fracture-controlled high temperature dolomites in the Cretaceous Ramales Formation (Cantabrian Mountain Chain, NW Spain); implications for reservoir characterization
American Association of Petroleum Geologists and Society for Sedimentary Geology; Tulsa, OK; USA; Un, 2010
2010 AAPG annual convention & exhibition; abstracts volume; Unmasking the potential of exploration & production
Ver registro

3.-  Geomatics; a key component of managing the Guarani aquifer system
Canadian Institute of Geomatics; Ottawa, ON; CAN; Canada, 2008
Ver registro

4.-  Influence of subduction zone structure on coastal and inland attenuation in Mexico
Wiley-Blackwell on behalf of The Royal Astronomical Society, the Deutsche Geophysikalische Gesellsch, 2009
Ver registro

5.-  INSLAB EARTHQUAKES OF CENTRAL MEXICO; PEAK GROUND-MOTION PARAMETERS AND RESPONSE SPECTRA
SEISMOLOGICAL SOCIETY OF AMERICA; BERKELEY, CA; USA; UNITED STATES, 2005
Ver registro

6.-  INSLAB EARTHQUAKES OF CENTRAL MEXICO; Q, SOURCE SPECTRA, AND STRESS DROP
SEISMOLOGICAL SOCIETY OF AMERICA; BERKELEY, CA; USA; UNITED STATES, 2004
Ver registro

7.-  IN-SLAB EARTHQUAKES OF CENTRAL MEXICO; Q, SOURCE SPECTRA, AND STRESS DROP
SEISMOLOGICAL SOCIETY OF AMERICA; EL CERRITO, CA; USA; UNITED STATES, 2004
SSA 2004; ABSTRACTS OF THE ANNUAL MEETING
Ver registro

8.-  Timing and structural evolution of an accretionary orogen, Northern Andes
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
Ver registro


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