Experiments on the simultaneous partitioning of divalent cations between arsenopyrite or cobaltite and hydrothermal chloride solution under supercritical conditions
Author:
Affiliation:
1. Faculty of Science and Engineering, Waseda University
Publisher
Japan Association of Mineralogical Sciences
Subject
Economic Geology,Geochemistry and Petrology
Link
https://www.jstage.jst.go.jp/article/gkk/48/3/48_181112/_pdf
Reference13 articles.
1. Bayliss, P. (1969): X-ray data, optical anisotropism, and thermal stability of cobaltite, gersdorffite, and ullmannite. Mineral. Mag., 37, 26-33.
2. Brimhall, G.H. and Crear, D.A. (1987): Ore fluids: Magmatic to supergene. In Thermodynamic modelling of geological materials: Minerals, fluids and melts (Carmichael, I.S.E. and Eugster, H.P. Eds). Reviews in Mineralogy 17, Mineral. Soc. Amer., Washington, D.C., 235-321.
3. Brostigen, G., Kjekshus, A. and Rømming, Chr. (1973): Compounds with the marcasite type crystal structure. Acta Chemi. Scandinavica, 27, 2791-2796.
4. Buerger, M.J. (1936): The symmetry and crystal structure of the minerals of the arsenopyrite group. In Crystalline Materials (Evgeny, A. et al., Eds.). Zeitschrift für Kristallographie, 95, 83-113.
5. Burnes, R.G. (1970): Mineralogical applications of crystal field theory. pp. 224, Cambridge Univ. Press, London
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