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Reconnaissance geology of the Mississippian Leadville limestone and implications for mineralization controls, Fulford mining district, Eagle County, ColoradoRichards, Billy D January 2011 (has links)
Typescript (photocopy). / Digitized by Kansas State University Libraries
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Geologic and economic study of ultramafic complexes of the coast of Guerrero, MexicoDelgado-Argote, Luis Alberto, 1953- January 1986 (has links)
No description available.
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Geology and geochemistry of Proterozoic volcanic rocks bearing massive sulfide ore deposits, Bagdad, ArizonaRobison, Lori Carol, 1955- January 1987 (has links)
No description available.
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Ore controls of the San Xavier mine, Pima County, ArizonaWilson, Clyde August, 1932- January 1960 (has links)
No description available.
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The geology and mineralization of the Sedimentary Hills Area, Pima County, ArizonaBennett, Paul J. (Paul Jerome), 1934- January 1957 (has links)
No description available.
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The geology and mineralization of the Northern Plomosa District, La Paz County, ArizonaDuncan, John Towner, 1960- January 1990 (has links)
No description available.
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The secondary dispersion of tungsten in some southern Arizona tungsten districtsFredericksen, Rick Stewart, 1949- January 1974 (has links)
No description available.
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Economic geology of the Alamos Mining District, Sonora, MexicoVazquez Perez, Adalberto, 1944- January 1975 (has links)
No description available.
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A comparison of churn and diamond drilling in the Quijotoa mining district, Pima county, ArizonaArozena, Joe de January 1917 (has links)
No description available.
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Cloning, Sequencing and Partial Characterization of the Accessory Gene Region of Plasmid pTC-F14 isolated from the Biomining Bacterium Acidithiobacillus caldus f.Goldschmidt, Gunther Karl 03 1900 (has links)
Thesis (MSc (Microbiology))--University of Stellenbosch, 2005. / Plasmid pTC-F14 is a 14.2kb promiscuous, broad-host range IncQ-like mobilizable plasmid isolated from Acidithiobacillus caldus f. At. caldus is a member of a consortium of bacteria (along with Acidithiobacillus ferrooxidans and Leptospirilum ferrooxidans) that is used industrially for decomposing metal sulphide ores and concentrates at temperatures of 40ºC or below which is now a well-established industrial process to recover metals from certain copper, uranium and gold-bearing minerals or mineral concentrates. These biomining microbes are usually obligately acidophilic, autotrophic, usually aerobic iron- or sulphur-oxidizing chemolithotrophic bacteria. Their remarkable physiology allows them to inhabit an ecological niche that is largely inorganic and differs from those environments populated by the more commonly studied non-acidophilic heterotrophic bacteria. At. caldus, is a moderately thermophilic (45 to 50ºC), highly acidophilic (pH1.5 to 2.5) sulphur-oxidizing bacterium, and its role as one of the major players in the industrial decomposition of metal sulphide ores has become evident in recent years. At. caldus f from which pTC-F14 was isolated was found to be one of two dominant organisms in a bacterial consortium undergoing pilot-scale testing for the commercial extraction of nickel from ores.
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