Geochemical Peculiarities of Galena and Sphalerite from Polymetallic Deposits of the Dal’negorskii Ore Region (Primorsky Krai, Russia)
- 10 Downloads
New data on the composition of the major minerals from the skarn and vein polymetallic deposits of the Dal’negorskii ore region are reported. Analysis of galena and sphalerite was carried out by the X-ray fluorescent energy-dispersive method of synchrotron radiation for the first time. It is shown that the minor elements in major minerals of different deposits are typomorphic. Among these elements are Fe, Cu, Ni, Cd, Ag, Sn, and Sb, as well as In in sphalerite and Te in galena. The high concentrations of Ag, Cu, Te, Cd, and In in the extracted minerals indicate the complex character of mineralization. The compositional patterns of ore minerals characterize the sequence of mineral formation from the skarn to vein ores, and the sequence of deposits from the mesothermal to epithermal conditions. This provides geochemical evidence for the stage model of the formation of mineralization in the Dal’negorskii ore region.
Unable to display preview. Download preview PDF.
- 1.V. A. Baskina, I. N. Tomson, M. M. Arakelyants, et al., Dokl. Earth Sci. 399 (8), 1051–1054 (2004).Google Scholar
- 2.V. A. Baskina, V. A. Lebedev, and I. N. Tomson, Dokl. Earth Sci. 405 (8), 1145–1149 (2005).Google Scholar
- 3.Geodynamics, Magmatism and Metallogeny of East Russia, Ed. by A. I. Khanchuk (Dal’nauka, Vladivostok, 2006) [in Russian].Google Scholar
- 4.M. G. Dobrovol’skaya and T. N. Shadlun, Mineral Associations and Formation Conditions of Lead-Zinc Ores (Nauka, Moscow, 1974) [in Russian].Google Scholar
- 5.M. G. Dobrovol’skaya, Lead-Zinc Metallization (Ore Formation, Mineral Parageneses, Features of Ore Formation) (Nauka, Moscow, 1989) [in Russian].Google Scholar
- 6.M. G. Dobrovol’skaya, S. P. Balashova, O. N. Zaozerina, et al., Geol. Rudn. Mestorozhd. 35 (6), 493–519 (1993).Google Scholar
- 7.V. V. Ivanov, Geochemistry of Trace Elements in Hydrothermal Deposits (Nedra, Moscow, 1966) [in Russian].Google Scholar
- 8.V. G. Moiseenko and L. I. Rogulina, Dokl. Earth Sci. A 389 (3), 392–394 (2003).Google Scholar
- 9.L. I. Rogulina, V. A. Kropotin, and E. N. Voropaeva, Litosfera, No. 3, 109–115 (2007).Google Scholar
- 11.L. I. Rogulina, O. L. Sveshnikova, and E. N. Voropaeva, Zap. Ross. Mineral. O-va 139 (4), 29–40 (2010).Google Scholar
- 12.L. I. Rogulina, V. I. Terebilo, V. G. Nevstruev, et al., in Proc. All-Russ. Sci. Pract. Conf. (Ammosov North- Eastern Federal Univ., Yakutsk, 2015), pp. 401–404 [in Russian].Google Scholar