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Wasson, J.T. and Kimberlin, J. (1967) The chemical classification of iron meteorites, II. Irons and pallasites with gemanium concentrations between 8 and 100 ppm. Geochimica et Cosmochimica Acta: 31: 2070.

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Year1967
Original EntryWasson, J.T. and Kimberlin, J. (1967) The chemical classification of iron meteorites, II. Irons and pallasites with gemanium concentrations between 8 and 100 ppm. Geochimica et Cosmochimica Acta: 31: 2070.
Mindat Ref. ID16330716Long-form Identifiermindat:1:5:16330716:3
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Full ReferenceWasson, J.T. and Kimberlin, J. (1967) The chemical classification of iron meteorites, II. Irons and pallasites with gemanium concentrations between 8 and 100 ppm. Geochimica et Cosmochimica Acta: 31: 2070.
Plain TextWasson, J.T. and Kimberlin, J. (1967) The chemical classification of iron meteorites, II. Irons and pallasites with gemanium concentrations between 8 and 100 ppm. Geochimica et Cosmochimica Acta: 31: 2070.

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Canyon City meteorite, Canyon City, Canyon Creek Mining District, Klamath Mountains, Trinity County, California, USA

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Wasson, J.T. and Kimberlin, J. (1967) The chemical classification of iron meteorites, II. Irons and pallasites with gemanium concentrations between 8 and 100 ppm. Geochimica et Cosmochimica Acta: 31: 2068.
Wasson, John T., Kimbeblin, Jerome (1967) The chemical classification of iron meteorites—II. Irons and pallasites with germanium concentrations between 8 and 100 ppm. Geochimica et Cosmochimica Acta, 31 (10) 2065-2093 doi:10.1016/0016-7037(67)90143-3
Scott, E.R.D., Wasson, J.T. and Buchwald, V.F. (1973) The chemical classification of iron meteorites, VII. A reinvestigation of irons with Ge concentrations between 25 and 80 ppm. Geochimica et Cosmochimica Acta, 1957
Scott, E.R.D., Wasson, J.T. and Buchwald, V.F. (1973) The chemical classification of iron meteorites, VII. A reinvestigation of irons with Ge concentrations between 25 and 80 ppm. Geochimica et Cosmochimica Acta, 1957-1983
Wasson, John T. (1969) The chemical classification of iron meteorites—III. Hexahedrites and other irons with germanium concentrations between 80 and 200 ppm. Geochimica et Cosmochimica Acta, 33 (7) 859-876 doi:10.1016/0016-7037(69)90032-5
Scott, Edward R.D, Wasson, John T, Buchwald, V.F (1973) The chemical classification of iron meteorites—VII. A reinvestigation of irons with Ge concentrations between 25 and 80 ppm. Geochimica et Cosmochimica Acta, 37 (8) 1957-1983 doi:10.1016/0016-7037(73)90151-8
Wasson, John T. (1967) The chemical classification of iron meteorites: I. A study of iron meteorites with low concentrations of gallium and germanium. Geochimica et Cosmochimica Acta, 31 (2) 161-180 doi:10.1016/s0016-7037(67)80043-7
Schaudy, R., Wasson, J.T., and Buchwald, V.F. (1972) The chemical classification of iron meteorites, VI. A reinvestigation of irons with Ge concentrations lower than 1 ppm. Icarus: 17: 174-192
Wasson, J.T. (1970) The chemical composition of meteorites, IV. Irons with Ge concentrations greater than 190 ppm and other meteorites associated with Group I. Icarus, 12: 410.
Wasson, J.T. (1970) The chemical composition of meteorites, IV. Irons with Ge concentrations greater than 190 ppm and other meteorites associated with Group I. Icarus, 12: 407-423.
Edward R. D. Scott & John T. Wasson (1976) Chemical classification of iron meteorites—VIII. Groups IC, IIE, IIIF and 97 other irons. Geochimica et Cosmochimica Acta 49 (1): 103-115. (Jan 1976).
 
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