Dualistic distribution coefficients of trace elements in the system mineral–hydrothermal solution. IV. Platinum and silver in pyrite

Author:

Tauson V. L.,Lipko S. V.,Arsent’ev K. Yu.,Mikhlin Yu. L.,Babkin D. N.,Smagunov N. V.,Pastushkova T. M.,Voronova I. Yu.,Belozerova O. Yu.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Reference47 articles.

1. P. K. Abraitis, R. A. D. Pattrick, and D. J. Vaughan, “Variations in the compositional, textural and electrical properties of natural pyrite: a review,” Int. J. Miner. Process. 74, 41–59 (2004).

2. J. G. Arnason, D. K. Bird, S. Bernstein, and P. B. Kelemen, “Gold and platinum-group element mineralization in the Kruuse Fjord Gabbro Complex, East Greenland,” Econ. Geol. 92 (4), 490–501 (1997).

3. K. Yu. Arsent’ev, V. L. Tauson, and S. V. Lipko, “Phenomena of nanophase aggregation and phase segregation of trace elements on the surface of crystals of ore minerals in multicomponent hydrothermal systems,” Vopr. Estestvozn., 2 (6), 14–18 (2015).

4. H. Bari, F. Cesbron, Y. Moelo, F. Permingeat, P. Picot, R. Pierrot, H.-J. Schubnel, and R. Weil, “Dervillite, Ag2AsS2, new definition,” Bull. Miner. 106 (5), 519–524 (1983).

5. A. V. Bochkarev, A. N. Trefilova, M. F. Bobrov, and N. A. Tsurkov, “Isotope separation during ionic crystal growth from solution,” Russ. J. Phys. Chem. A 77 (11), 1868–1872 (2003).

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