Abstract
Electronprobe microanalyses were made of enargite and luzonite from various localities. It was shown that enargite can contain as much as 6 wt.% antimony. Complete solid solution was observed between the tetragonal phases luzonite and famatinite. The compositions of enargite and of luzonite-famatinite solid solution were found to be very variable even within one polished section.
Zusammenfassung
Anhand quantitativer Elektronenstrahl-Mikroanalysen von Material verschiedener Lagerstätten wurde festgestellt, daß Enargit bis zu 6 Gew.% Antimon enthalten kann. Zwischen den tetragonalen Phasen Luzonit und Famatinit wurde völlige Mischbarkeit beobachtet. Es wurde gefunden, daß die Zusammensetzung von Enargit und Luzonit-Famatinit selbst im Bereich eines Anschliffes stark schwanken kann.
References
Gaines, R. V.: Luzonite, famatinite and some related minerals. Am. Mineralogist 42, 766–779 (1957).
Levy, C.: Contribution à la minéralogie des sulfures de cuivre du type Cu3XS4. Mém. Bur. Rech. Géol. Minières 54, 101–124 (1967).
Skinner, B. J.: Assemblage enargite-famatinite, a possible geologic thermometer. (abstr.) Bull. Geol. Soc. Am. 71, 1975 (1959). See also P. B. Barton Jr. and B. J. Skinner: Sulfide mineral stabilities. In H. L. Barnes (ed.): Geochemistry of hydrothermal ore deposits, p. 306. New York: Holt, Rinehard and Winston 1967.
Springer, G.: Die Berechnung von Korrekturen für die quantitative Elektronenstrahl-Mikroanalyse. Fortschr. Mineral 45, 103–124 (1967).
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Temporary address (1968/69): Department of Mineral Technology, Imperial College, London S. W. 7, England.
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Springer, G. Compositional variations in enargite and luzonite. Mineral. Deposita 4, 72–74 (1969). https://doi.org/10.1007/BF00206649
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DOI: https://doi.org/10.1007/BF00206649