Geochemistry alteration

Scratch, R.B., Watson, G.P., Kerrich, R. Hutchinson, R.W. (1984) Fracture controlled antimony-quartz mineralization. Lake George Deposit, New Brunswick mineralogy, geochemistry, alteration, and hydrothermal regimes. Econ. Geol. Bull. Soc. Econ. Geol., 79, 1159-1186. 

Tuross, N., Behrensmeyer, A.K., Eanes, E.D., Fisher, L.W. and Hare, P.E. 1989 Molecular preservation and crystallographic alterations in a weathering sequence of wildebeest hones. Applied Geochemistry 4 261-270. 

Roulet M, Lucotte M, Saint-Aubin A, Tran S, Rheault I, Farella N, de Jesus da Silva E, Dezencourt J, Sousa Passes CJ, Santos Soares G, Guimaraes JR, Mergler D, Amorim M. 1998. The geochemistry of mercury in central Amazonian soils developed on the Alter-do-Chao formation of the lower Tapajos River valley, Para state, Brazil. Sci Total Environ 223 1-24. 

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. 

Kawahata, H., Kusakabe, M. and Kikuchi, Y. (1987) Strontium, oxygen, and hydrogen isotope geochemistry of hydrothermally altered and weatherted rocks in DSDP Hole 504B, Costa Rica Rift. Earth Planet. 

Meyer, C. and Hemley, J.J. (1967) Wall rock alteration. In Barnes, H.L., (ed.). Geochemistry of Hydrothermal Ore Deposits, Holt Rinehart Winston, pp. 166-235. 

Shikazono, N. (1999a) Rare earth element geochemistry of Kuroko ores and altered rocks implication for evolution of submarine geothermal system at back-arc basin. Resource Geology Special Issue, 20,... 

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. 

Stakes, D.S. and O Neil, Jr. (1982) Mineralogy and stable i.sotopes geochemistry of hydrothermally altered ocean rocks. Earth Planet. Sci. Lett, 57, 285-304. 

Marumo, K. and Hattori, K.H. (1997) Seafloor hydrothermal clay alteration at Jade in the back-arc Okinawa Trough Mineralogy, geochemistry and isotope characteri.stics. Geochim. Cosmochim. Acta, 63, 2785-2804. 

Shikazono, N. (1999) Rare earth element geochemistry of Kuro ores and hydrothermaily altered rocks Implication for the evolution of submarine hydrothermal systems at back-arc basins. Resource Geol. Spec. Issue, 20, 23-30. 

Salzsauler, K. A., Sherriff, B.L., Sidenko, N.V. 2005. As mobility in alteration products of sulfide-rich, arsenopyrite-bearing mine wastes, Snow Lake, Manitoba, Canada. Applied Geochemistry, 20, 2303-2314. Simpson, S. 2007 The Source, Attenuation and Potential Mobility of As at New Britannia Gold Mine, Snow Lake, Manitoba. M.Sc Thesis, University of Manitoba. 

Wakeham, S.G., and C. Lee. 1993. Production, transport, and alteration of particulate organic matter in the marine water column. Pp. 145-169 in Organic Geochemistry Principles and Applications, M.H. Engle and S.A. Macko, eds., New York Plenum Press. 

The first substantive report of Li isotopes in any Earth materials (Chan and Edmond 1988) largely presaged what was to come in Li isotope research in the oceans. The interpretations therein, based on a handful of data from seawater, fresh and altered basalt, hydrothermal fluids and lake waters, laid out the foundation to what has come since, in terms of natural and laboratory-based studies of the marine geochemistry of Li isotopes. 

One of the main applications of hydrogen and oxygen isotope thermometry in geochemistry is the estimation of the reservoir temperatures of active geothermal systems or the evaluation of the ruling T conditions during deposition or alter-... 

Norman, D.K., Parry, W.T., Bowman, J.R. 1991. Petrology and Geochemistry of Propylitic Alteration at Southwest Tintic, Utah. Economic Geology, 86, 13-28. 

The lithogeochemistry of wall rocks in the Hollinger-Mcintyre-Coniaurum (HMC) deposit has not been fully explored. The objective of this study was to characterize the lithogeochemical alteration of the wall rocks and the stable isotope geochemistry of the veins in order to (1) test if the HMC deposit is zoned chemically (2) determine how many mineralizing events were involved in forming the HMC deposit and (3) identify fluid pathways involved in formation of the HMC gold deposit. 

Smith, T.J. Kesler, S.E. 1985. Relation of fluid inclusion geochemistry to wallrock alteration and lithological zonation at the Hollinger-Mcintyre gold deposit, Timmins, Ontario. Canadian Institute of Mining Bulletin, 78, 35-46. 

---