| Registros del 1 al 9 de 9 encontrados |
1.- CHARACTERIZATION AND ORIGIN OF FE (SUPER 3+) -MONTMORILLONITE IN DEEP-WATER CALCAREOUS SEDIMENTS (PACIFIC OCEAN, COSTA RICA MARGIN)
CLAY MINERALS SOCIETY; CLARKSON, NY; USA; UNITED STATES, 2005
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2.- Chlorite alteration and its relationship with gold mineralization in the Fazenda Brasileiro orogenic gold deposit, Bahia, Brazil
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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3.- Clay minerals related to circulation of near neutral to weakly acidic fluids in active high energy geothermal systems
Societe Geologique de France; Paris; FRA; France, 2010
Hydrothermalisme en domaine continental ;Hydrothermalism in the continental domain
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4.- FLUID-ROCK INTERACTION IN THE GEOTHERMAL FIELD OF CHIPILAPA (EL SALVADOR); CONTRIBUTION OF FLUID-INCLUSION DATA
SCHWEIZERBART'SCHE VERLAGSBUCHHANDLUNG (NAEGELE U. OBERMILLER); STUTTGART; DEU; FEDERAL REPUBLIC OF , 1996
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5.- Metamorphic evolution of Weber Belt and timing of gold mineralization in Fazenda Brasileiro gold deposit, Bahia, Brazil by Ar (super 40) -Ar (super 39) on amphiboles
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
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6.- Middle Permian telodiagenetic processes in Neoproterozoic sequences, Tandilia System, Argentina
Society for Sedimentary Geology; Tulsa, OK; USA; United States, 2007
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7.- Petrography and chemistry of SiO (sub 2) filling phases in the amethyst geodes from the Serra Geral Formation deposit, Rio Grande do Sul, Brazil
Elsevier; Oxford; GBR; United Kingdom, 2010
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8.- ROLE OF THE DEPOSITIONAL ENVIRONMENT ON CLAY DIAGENESIS; EXAMPLE OF THE LOWER CRETACEOUS OF THE BASCO-CANTABRIAN BASIN (NORTHERN SPAIN)
SOCIETE GEOLOGIQUE DE FRANCE; PARIS; FRA; FRANCE, 2000
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9.- Spatial and temporal evolution of hydrothermal alteration at Lavras do Sul, Brazil; evidence from dioctahedral clay minerals
Clay Minerals Society; Clarkson, NY; USA; United States, 2008
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