Instituto Geológico y Minero de España

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Instituto Geológico y Minero de España
 Registros del al 10 de 259 encontrados

1.-  A CENTURY OF FIRE AND BRIMSTONE; THE RISE AND FALL OF THE FRASCH SULPHUR INDUSTRY OF THE GULF OF MEXICO BASIN
GEOLOGICAL SOCIETY PUBLISHING HOUSE; BATH; GBR; UNITED KINGDOM, 2002
INDUSTRIAL MINERALS AND EXTRACTIVE INDUSTRY GEOLOGY
Ver registro

2.-  A new model for the evolution of diamond-forming fluids
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2009
European Geosciences Union general assembly 2009
Ver registro

3.-  A NEW TETRAGONAL SILICATE MINERAL OCCURRING AS INCLUSIONS IN LOWER-MANTLE DIAMONDS
MACMILLAN JOURNALS; LONDON; GBR; UNITED KINGDOM, 1997
Ver registro

4.-  A RIFT MODEL FOR THE SEDIMENTARY DIAMOND DEPOSITS OF BRAZIL
SPRINGER-VERLAG; BERLIN; DEU; FEDERAL REPUBLIC OF GERMANY, 1998
Ver registro

5.-  A TWO-STAGE PROCESS OF NATIVE PALLADIUM FORMATION AT LOW TEMPERATURES; EVIDENCE FROM A PALLADIAN GOLD NUGGET (GONGO SOCO IRON ORE MINE, MINAS GERAIS, BRAZIL)
MINERALOGICAL SOCIETY; LONDON; GBR; UNITED KINGDOM, 2003
Ver registro

6.-  Alluvial diamonds from the Rio Soriso (Juina, Brazil)
Geological Association of Canada; Waterloo, ON; CAN; Canada, 2003
Geological Association of Canada, Mineralogical Association of Canada; joint annual meeting; abstracts--Association geologique du Canada, Association mineralogique du Canada; congres annuel conjointe; recueil des resumes
Ver registro

7.-  Anatexis and melt extraction in the pelitic crust; how does it look down there?
American Geophysical Union; Washington, DC; USA; United States, 2006
AGU 2006 fall meeting
Ver registro

8.-  Ancient graphite in the Eoarchean quartz-pyroxene rocks from Akilia in southern West Greenland; II, Isotopic and chemical compositions and comparison with Paleoproterozoic banded iron formations
Elsevier; New York, NY; III; International, 2010
Ver registro

9.-  Anticorrelation between low delta (super 13) C of eclogitic diamonds and high delta (super 18) O of their coesite and garnet inclusions requires a subduction origin
Geological Society of America (GSA); Boulder, CO; USA; United States, 2013
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10.-  ARE SOME OF THE DEEP CRUSTAL CONDUCTIVE FEATURES FOUND IN SW IBERIA CAUSED BY GRAPHITE?
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2002
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