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Mineralogy/mining

In Table IV, the data given in Table II are projected to the revenue targets that we now consider are realistic for each of these mines using the Warner Process system. The projected improvements in revenue will, of course, be further increased by the cost savings possible in operations. As one would expect, the mines that stand to gain the most are those wife the more complex ore mineralogy. Mine No. 9 is on an ore that contains significant amounts of cobalt in... [Pg.672]

Charles Friedel (1832-1899) was horn in Strasbourg, France, and studied at the Sorbonne in Paris. Trained as both 3 mineralogist and a chemist, he was among the first to attempt to manufacture synthetic diamonds. He was professor of mineralogy at the School of Mines before becoming professor of chemistry at the Sorbonne (1884-1899). [Pg.555]

Bryndzia, L.T., Scott, S.D. and Farr, J.E. (1983) Mineralogy, geochemistry, and mineral chemistry of siliceous ore and altered footwall rocks in the Uwamuki 2 and 4 deposits, Kosaka mine, Hokuroku district, Japan. Econ. GeoL Mon., 5, 507-522. [Pg.269]

Nakamura, T. (1963) On some characteristic mineralogical features of chlorite from the Ashio copper mine, Japan. J. Geosci. Osaka City U., 7, 97-111. [Pg.281]

Shikazono, N. (1985a) Mineralogical and fluid inclusion features of rock alterations in the Seigoshi gold-silver mining district, western part of Izu Peninsula, Japan. Ghent. Geol, 213-230. [Pg.286]

Shikazono, N., Nakata, M. and Shimizu, M. (1990) Geochemical, mineralogic and geologic characteristics of Se- and Te-bearing epithermal gold deposits in Japan. Mining Geology, 40, 337-352. [Pg.287]

Shikazono, N., Utada, M. and Shimizu, M. (1995) Mineralogical and geochemical characteristics of hydrothermal alteration of basalt in the Kuroko mine area, Japan Implications for the evolution of back arc basin hydrothermal system. Applied Geochemistry, 10, 621-642. [Pg.287]

Pigna M, Colombo C, Violante A (2003) Competitive sorption of arsenate and phosphate on synthetic hematites (in Italian). Proceedings XXI Congress of Societa Italiana Chimica Agraria SICA (Ancona), pp 70-76 Quirk JP (1955) Significance of surface area calculated from water vapour sorption isotherms by use of the B. E. T. equation. Soil Sci 80 423-430 Rancourt DG, Fortin D, Pichler T, Lamarche G (2001) Mineralogical characterization of a natural As-rich hydrous ferric oxide coprecipitate formed by mining hydrothermal fluids and seawater. Am Mineral 86 834-851 Raven K, Jain A, Loeppert, RH (1998) Arsenite and arsenate adsorption on ferrihydrite kinetics, equilibrium, and adsorption envelopes. Environ Sci Technol 32 344-349... [Pg.67]

Adamo, P., S. Dudka, M.J. Wilson, and WJ. McHardy. 1996. Chemical and mineralogical forms of Cu and Ni in contaminated soils from the Sudbury mining and smelting region, Canada. Environ. Pollut. 91 11-19. [Pg.519]

Jambor, J.L. 2003. Mine waste mineralogy and mineralogical perspectives of acid-base accounting. In Jambor, J.L., Blowes, D.W., Ritchie, A.M.I. (eds.), Environmental aspects of mine waste, Mineralogical Association of Canada Short Course, 31, 117-147. [Pg.132]

Jambor, J.L. Blowes, D.W. 1994. Environmental Geochemistry of Sulfide Mine-Wastes. Mineralogical Association of Canada Short Course 22, 438 p. [Pg.318]


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Mineralogy and mining

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