Reference | {Deposit:: Albers, J.P. and Bain, J.H.C., 1985, Regional setting and new information on some critical geologic features of the West Shasta District, California: Economic Geology, v. 80, p. 2072-2091.}{Deposit:: Averill, C.V., 1939, Mineral resources of Shasta County: California Journal of Mines and Geology, v. 35, no. 2, p. 108-191.}{Deposit:: Bence, A.E. and Taylor, B.E., 1985, Rare earth element systematics of West Shasta metavolcanics rocks: petrogenesis and hydrothermal alteration: Economic Geology, v. 80, p. 2164-2176.}{Deposit:: Brown, G.C., 1915, The counties of Shasta, Siskiyou, Trinity: California State Mining Bureau 14th Report of the State Mineralogist, p. 767-769.}{Deposit:: Doe, B.R. and others, 1985, The plumbotectonics of the West Shasta Mining District, California: Economic Geology, v. 80, p. 2136-2148.}{Deposit:: Fraticelli, L.A. and others, 1987, Geologic map of the Redding 1 x 2 degree quadrangle: Shasta, Tehama, Humboldt, and Trinity counties, California: U.S. Geological Survey Open-File Report 87-257, scale 1:250,000.}{Deposit:: Guilbert, J.M. and Park, C.F., Jr., 1986, The geology of ore deposits: W.H. Freeman and Company, New York, p. 589-595.}{Deposit:: Hassemer, J.R., 1983, Some preliminary findings of a reconnaissance geochemistry study, West Shasta District, California: U.S. Geological Survey Open-File Report 83-57, 16 p.}{Deposit:: Horton, R.J. and others, 1985, Electrical geophysical investigations of massive sulfide deposits and their host rocks, West Shasta Copper-Zinc District: Economic Geology, v. 80, p. 2213-2229.}{Deposit:: Howe, S.S., 1985, Mineralogy, textures, and relative age relationships of massive sulfide ore in the West Shasta District, California: Economic Geology, v. 80, p 2114-2127.}{Deposit:: Huston, D.L., and others, 1996, Productivity of volcanic-hosted massive sulfide districts: New constraints from the d18O of quartz phenocrysts in cogenetic felsic rocks: Geology, v. 24, P. 459-462.}{Deposit:: Hutchinson, R.W. and Albers, J.P., 1992, Metallogenic evolution of the Cordilleran region of the western United States, in Burchfiel, B.C. and others, editors, The Cordilleran Orogen: Conterminous U.S.: Geological Society of America, The Geology of North America, v. G-3. p. 629-652.}{Deposit:: Irwin, W.P., 1981, Tectonic accretion of the Klamath Mountains, in Ernst, W.G., editor, The geotectonic development of California: Prentice-Hall, Englewood Cliffs, New Jersey, p. 29-49.}{Deposit:: Irwin, W.P., 1994, Geologic map of the Klamath Mountains, California and Oregon: U.S. Geological Survey MIS Map I-2148, scale 1:500,000.}{Deposit:: Irwin, W.P. and Mankinen, E.A., 1998, Rotational and accretionary evolution of the Klamath Mountains, California and Oregon, from Devonian to present time: U.S. Geological Survey Open-File Report 98-114.}{Deposit:: Jenkins, O.P., 1948, Copper in California: California Division of Mines Bulletin 144, p. 334.}{Deposit:: Kinkel, A.R., Jr. and Hall, W.E., 1952, Geology of the Mammoth Mine, Shasta County, California: California Division of Mines Special Report 28, 16 p.}{Deposit:: Kinkel, A.R., Jr. and others, 1956, Geology and base-metal deposits of West Shasta Copper-Zinc District, Shasta County, California: U.S. Geological Survey Professional Paper 285, 156 p.}{Deposit:: Kinkel, A.R. and Kinkel, A.R., Jr., 1966, Copper, in Albers, J.P., editor, Mineral resources of California: California Division of Mines and Geology Bulletin 191, p.141-150.}{Deposit:: Kistler, R.W. and others, 1985, A reconnaissance Rb-Sr, Sm-Nb, U-Pb, and K-Ar study of some host rocks and ore minerals in the West Shasta Cu-Zn District, California: Economic Geology, v. 80, p. 2128-2135.}{Deposit:: Lapierre, H. and others, 1985, Geodynamic setting of early Devonian Kuroko-type sulfide deposits in the eastern Klamath Mountains (Northern California) inferred by the petrological and geochemical characteristics of the associated island-arc volcanic rocks: Economic Geology, v. 80, p. 2100-2113.}{Deposit:: Lindberg, P.A., 1985, A volcanogenic interpretation for massive sulfide origin, West Shasta District, California: Economic Geology, v. 80, p. 2240-2254.}{Deposit:: Lydon, P.A. and O?Brien, J.C., 1974, Mines and mineral resources of Shasta County, California: California Division of Mines and Geology County Report 6, 154 p.}{Deposit:: Miller, E.L. and others, 1992, Late Paleozoic paleogeographic and tectonic evolution of the western U.S. Cordillera, in Burchfiel, B.C. and others, editors, The Cordilleran Orogen: Conterminous U.S.: Geological Society of America, The Geology of North America, v. G-3. p. 57-106.}{Deposit:: O?Brien, J.C., 1957, Copper, in Wright, L.A., editor, Mineral commodities of California: California Division of Mines Bulletin 176, p.169-182.}{Deposit:: Poole, F.G. and others, 1992, Latest Precambrian to latest Devonian time; Development of a continental margin, in Burchfiel, B.C. and others, editors, The Cordilleran Orogen: Conterminous U.S.: Geological Society of America, The Geology of North America, v. G-3. p. 9-56.}{Deposit:: Potter, A.W. and others, 1990, Early Paleozoic stratigraphic, paleogeographic, and biogeographic relations of the eastern Klamath belt, northern California, in Harwood, D.S. and Miller, M.M., editors, Paleozoic and early Mesozoic paleogeographic relations; Sierra Nevada, Klamath Mountains, and related terranes: Geological Society of America Special Paper 255, p. 57-74.}{Deposit:: Raines, G.L. and others, 1985, Near-infrared spectra of West Shasta gossans compared with true and false gossans from Australia and Saudi Arabia: Economic Geology, v. 80, p. 2230-2239.}{Deposit:: Reed, M.H., 1984, Geology, wall-rock alteration, and massive sulfide mineralization in a portion of the West Shasta District, California: Economic Geology, v. 79, p. 1299-1318.}{Deposit:: Saleeby, J.B., 1992, Petrotectonic and paleogeographic settings of U.S. Cordilleran ophiolites, in Burchfiel, B. C. and others, editors, The Cordilleran Orogen: Conterminous U.S.: Geological Society of America, The Geology of North America, v. G-3. p. 653-682.}{Deposit:: Singer, D.A., 1986, Descriptive model of Kuroko massive sulfide, in Cox, D.P. and Singer, D.A., editors, Mineral deposit models: U.S. Geological Survey Bulletin 1693, p. 189-190.}{Deposit:: Stevens, C.H. and others, 1990, Significance of the provincial signature of Early Permian fauna of the eastern Klamath terrane, in Harwood, D.S. and Miller, M.M., editors, Paleozoic and early Mesozoic paleogeographic relations; Sierra Nevada, Klamath Mountains, and related terranes: Geological Society of America Special Paper 255, p. 201-218.}{Deposit:: Strand, R.G., 1962, Geologic atlas of California: Redding Sheet: California Division of Mines and Geology GAM 011, scale 1:250,000.}{Deposit:: Taylor, B.E. and South, B.C., 1985, Regional stable isotope systematics of hydrothermal alteration and massive sulfide deposition in the West Shasta District, California: Economic Geology, v. 80, p. 2149-2163.}{Deposit:: Tucker, W.B., 1926, Shasta County: California State Mining Bureau 22nd Report of the State Mineralogist, p. 121-216.}{Deposit:: Watkins, R. and Stensrud, H.L., 1983, Age of sulfide ores in the West Shasta and East Shasta Districts, Klamath Mountains, California: Economic Geology, v. 78, p. 340-343.}{Deposit:: Brown, G.C., 1913, Field report on Mammoth Mine (File Number 322-5690, CDMG Mineral Resources Files, Sacramento).} |