Registros del 1 al 10 de 259 encontrados |
![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 3.- A NEW TETRAGONAL SILICATE MINERAL OCCURRING AS INCLUSIONS IN LOWER-MANTLE DIAMONDS
MACMILLAN JOURNALS; LONDON; GBR; UNITED KINGDOM, 1997
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![](./images/clear.gif) 4.- A RIFT MODEL FOR THE SEDIMENTARY DIAMOND DEPOSITS OF BRAZIL
SPRINGER-VERLAG; BERLIN; DEU; FEDERAL REPUBLIC OF GERMANY, 1998
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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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![](./images/clear.gif) 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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