Instituto Geológico y Minero de España

LogoSistema de información documental - SID

 

 

 

Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 10 de 153 encontrados

1.-  2D magnetotelluric interpretation of the crust electrical resistivity across the Pampean Terrane-Rio de la Plata Suture, in central Argentina
Elsevier; Amsterdam; NLD; Netherlands, 2008
New insights into Andean evolution
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2.-  A 54 m thick loess profile in North Pampa, Argentina
[International Union for Quaternary Research];; III; International, 2003
XVI INQUA congress; shaping the Earth, a Quaternary perspective
Ver registro

3.-  A modern subtropical playa complex; Salina de Ambargasta, central Argentina
Elsevier; Oxford; GBR; United Kingdom, 2012
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4.-  A POSSIBLE TEKTITE STREWN FIELD IN THE ARGENTINIAN PAMPA
AMERICAN ASSOCIATION FOR THE ADVANCEMENT OF SCIENCE; WASHINGTON, DC; USA; UNITED STATES, 2002
Ver registro

5.-  AGE, SR- AND ND-ISOTOPE SYSTEMATICS, AND ORIGIN OF TWO FLUORITE LODES, SIERRAS PAMPEANAS, ARGENTINA
WINSTON & SON; SILVER SPRING, MD; USA; UNITED STATES, 1997
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6.-  Amphibole in vermiculite mined in Argentina; morphology, quantitative and chemical studies on the different phases of production and their environmental impact
Springer; Berlin; DEU; Germany, 2013
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7.-  ANALISIS HIDRODINAMICO, GEOQUIMICO E ISOTOPICO DE BASE PARA LA EVALUACION DE SISTEMAS HIDROTERMALES DE BAJA TEMPERATURA EN LA LLANURA CORDOBESA (ARGENTINA)
2010
NUMERO MONOGRAFICO. HIDROGEOLOGIA EN IBEROAMERICA
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8.-  ANALYSIS OF ARSENIC POLLUTION IN GROUNDWATER AQUIFERS BY X-RAY FLUORESCENCE
PERGAMON; OXFORD; III; INTERNATIONAL, 2001
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9.-  Anisotropy and mantle flow in the eastern Sierras Pampeanas from shear wave splitting
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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10.-  ANTHONY Z. HELMS AND HIS GEOLOGICAL OBSERVATIONS IN ARGENTINA DURING 1789
[INTERNATIONAL GEOLOGICAL CONGRESS]; [LOCATION VARIES]; III; INTERNATIONAL, 2000
BRAZIL 2000; 31ST INTERNATIONAL GEOLOGICAL CONGRESS; ABSTRACT VOLUME
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