Инд. авторы:	Rogulina L.I., Moiseenko V.G., Ponomarchuk V.A.
Заглавие:	Geochemical Peculiarities of Galena and Sphalerite from Polymetallic Deposits of the Dal’negorskii Ore Region (Primorsky Krai, Russia)
Библ. ссылка:	Rogulina L.I., Moiseenko V.G., Ponomarchuk V.A. Geochemical Peculiarities of Galena and Sphalerite from Polymetallic Deposits of the Dal’negorskii Ore Region (Primorsky Krai, Russia) // Doklady Earth Sciences. - 2018. - Vol.479. - Iss. 2. - P.468-471. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы:	DOI: 10.1134/S1028334X18040074; РИНЦ: 35485080; SCOPUS: 2-s2.0-85047273310; WoS: 000432735700013;
Реферат:	eng: 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. © 2018, Pleiades Publishing, Ltd.
Ключевые слова:	Ores; Stage models; Polymetallic; Ore minerals; Minor elements; Mineral formation; Geochemical evidence; Complex character; Zinc sulfide; Synchrotron radiation; Mineralogy; Geochemistry; Deposits; Energy dispersive method;
Издано:	2018
Физ. характеристика:	с.468-471
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