Instituto Geológico y Minero de España

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Instituto Geológico y Minero de España
 Registros del al 10 de 22 encontrados

1.-  A fractal interaction model for winding paths through complex distributions; application to soil drainage networks
Birkhaeuser; Basel; CHE; Switzerland, 2008
Earth sciences and mathematics; Volume 1
Ver registro

2.-  A MULTIVARIATE STATE-SPACE-MODEL APPROACH TO SPATIAL SAMPLING DESIGN
[PUBLISHER VARIES]; [LOCATION VARIES]; III; INTERNATIONAL, 1997
PROCEEDINGS OF IAMG '97, THE THIRD ANNUAL CONFERENCE OF THE INTERNATIONAL ASSOCIATION FOR MATHEMATICAL GEOLOGY
Ver registro

3.-  CONTRIBUTION A L'ETUDE THERMODYNAMIQUE DE L'ECHANGE D'IONS SODIUM-HEXYLAMMONIUM DANS DES VERMICULITES
1981
Ver registro

4.-  Entropy in natural time of geoelectric time series of dichotomic nature
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010
European Geosciences Union general assembly 2010
Ver registro

5.-  Entropy-based equation to assess hillslope sediment production
Wiley & Sons; Chichester; GBR; United Kingdom, 2007
Ver registro

6.-  ESTIMATING THE DISTRIBUTION OF PRIMARY REFLECTION COEFFICIENTS
SOCIETY OF EXPLORATION GEOPHYSICISTS; TULSA, OK; USA; UNITED STATES, 2003
Ver registro

7.-  EXPERIMENTAL AND EMPIRICAL INVESTIGATION OF THE SILVER SULFIDE-SILVER SELENIDE SYSTEM AND DISCRIMINATION OF TOPAZ RHYOLITES BY MAJOR-ELEMENT COMPOSITION
1995
Ver registro

8.-  FUZZY PARTITIONING SYSTEMS FOR ELECTROFACIES CLASSIFICATION; A CASE STUDY FROM THE MARACAIBO BASIN
SCIENTIFIC PRESS; BEACONSFIELD; GBR; UNITED KINGDOM, 2001
FIELD APPLICATIONS OF INTELLIGENT COMPUTING TECHNIQUES
Ver registro

9.-  Genetic features of peridotite-eclogite complexes in fold-belts and diamondiferous pipes in cratons
Zhonggno Dizhi Daxue; Beijing; CHN; China, 2007
Special issue on "Earth material science" (researches on mantle petrology and geochemistry)
Ver registro

10.-  INDUCCION DE HABITOS CRISTALINOS POR EFECTO DE ANISOTROPIA DEL APORTE. INFLUENCIA DE LA ENTROPIA DE SUPERFICIE;
1984
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