Instituto Geológico y Minero de España

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Instituto Geológico y Minero de España
 Registros del al 10 de 49 encontrados

1.-  A MAJOR HOLOCENE ENSO ANOMALY DURING THE MEDIEVAL PERIOD
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004
Ver registro

2.-  A pot experiment with mixtures of slate processing fines and compost
Elsevier; Amsterdam; NLD; Netherlands, 2007
Ver registro

3.-  ANALYTICAL CAVITY EXPANSION-CRITICAL STATE MODEL FOR PIEZOCONE DISSIPATION IN FINE-GRAINED SOILS
JAPANESE SOCIETY OF SOIL MECHANICS AND FOUNDATION ENGINEERING; TOKYO; JPN; JAPAN, 2002
Ver registro

4.-  Causes and consequences of bimodal grain-size distribution of tephra fall deposited during the August 2006 Tungurahua eruption (Ecuador)
Springer International [for the] International Association of Volcanology and Chemistry of the Earth, 2012
Ver registro

5.-  Characterization and geochemical-geotechnical properties of granite sawdust produced by the dimension stone industry of O Porrino (Pontevedra, Spain)
Geological Society of London; London; GBR; United Kingdom, 2010
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6.-  CONCENTRACION GRAVIMETRICA
1999
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7.-  Cycles and origin of ultrafine and black carbon particles in Huelva City (SW Spain)
Elsevier; New York, NY; III; International, 2009
Abstracts of the 19th annual V. M. Goldschmidt conference
Ver registro

8.-  DIMENSIONAL ANALYSIS OF MUD-RICH SEDIMENTARY DEPOSITS ON CONTINENTAL SHELVES
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2001
GEOLOGICAL SOCIETY OF AMERICA, 2001 ANNUAL MEETING
Ver registro

9.-  DISTAL ALLUVIAL LITHOFACIES AND THEIR TEXTURAL RESPONSES, SALDAN FORMATION (LOWER CRETACEOUS), CENTRAL ARGENTINA
INTERNATIONAL ASSOCIATION OF SEDIMENTOLOGISTS, COMPARATIVE SEDIMENTOLOGY DIVISION; UTRECHT; NLD; NET, 1994
14TH INTERNATIONAL SEDIMENTOLOGICAL CONGRESS; ABSTRACTS
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10.-  DUST DEVIL FLUX VARIABILITY DUE TO CHANGES IN DESERT SURFACE CONDITIONS
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2002
GEOLOGICAL SOCIETY OF AMERICA, 2002 ANNUAL MEETING
Ver registro


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