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Mineral assemblages of the porphyry tin-polymetallic ores of Mount Krasnaya paleovolcano of the Krasnogorsky deposit in the Dal’negorsk ore district

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Abstract

This paper presents the results of the detailed mineralogical study of the pocket-disseminated tinzinc (cassiterite-sulfide) and vein-metasomatic tin-silver-polymetallic ores localized in the vent of the Mount Krasnaya paleovolcano (Krasnogorsky polymetallic deposit). The tin-zinc ores of the early Late Maastrichtian stage of the ore formation are associated with pipelike bodies of explosion breccias, were formed at a temperature of around 300°C, and include three mineral assemblages: the (1) pyrite, (2) productive quartz-cassiterite-sphalerite, and (3) late sulfosalt-galena-chalcopyrite ones. The vein-metasomatic tin-silver-polymetallic ores of the late Paleocene stage are associated with rhyolite bodies, controlled by the NW-oriented faults, and cut mineralized breccia. These ores were formed during a full two-stage hydrothermal cycle within the temperature interval from 500 to 1000°C and include five consecutive ore mineral assemblages: (1) wolframite-arsenopyrite, (2) cassiterite-sphalerite-pyrite-chalcopyrite, (3) stannite-Ag-bearing sulfosalt, (4) freibergite-galena, and (5) native silver-stephanite-acanthite. The tin-silver-polymetallic ores are assumed to have formed simultaneously with the extended silver-bearing galena-sphalerite veins cutting the Primorskaya Group volcanic rocks around the paleovolcano. In the extended vein zones, the tinsilver-polymetallic ores correspond to the uppermost (closest to the paleosurface) part of the vertical zoning.

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References

  1. N. S. Bortnikov, O. N. Zaozerina, A. D. Genkin, and G. N. Muravitskaya, “Stannite-sphalerite as possible indicators of ore formation,” Geol. Rudn. Mestorozhd., No. 5, 32–44 (1990).

    Google Scholar 

  2. Geodynamics, Magmatism, and Metallogeny of East Russia, Ed. by A. I. Khanchuk (Dal’nauka, Vladivostok, 2006) [in Russian].

    Google Scholar 

  3. M. G. Dobrovol’skaya, S. P. Balashova, O. N. Zaozerina, and T. I. Golovanova, “Mineral assemblages and stages of ore formation in the lead-zinc deposits of the Dal’negorsk ore district, South Primorye,” Geol. Rudn. Mestorozhd. 32(5), 493–519 (1993).

    Google Scholar 

  4. I. Ya. Nekrasov, V. I. Sorokin, and E. G. Osadchii, “Iron and zinc distribution between sphalerite and stannite at T = 300–500°C and P = 1 kbar,” Dokl. Akad. Nauk SSSR 226(5), 116–1168 (1976).

    Google Scholar 

  5. “Main problems in study and mining of mineral raw material of the Far East economic region,” in FEER Mineral-Raw Complex at the Turn of Centuries (DVIMS, Khabarovsk, 1999) [in Russian].

  6. G. A. Osipova, Trace Elements and Mineral Microinclusions in the Cassiterites and Sulfides of Tin-Polymetallic Deposits (Dal’nauka, Vladivostok, 1993) [in Russian].

    Google Scholar 

  7. V. V. Ratkin, L. F. Simanenko, D. N. Kuznetsov, and R. V. Korol’, “Tin-zinc mineralization of the East Sikhote Alin volcanic belt,” Geol. Rudn. Mestorozhd. 32(2), 68–77 (1990).

    Google Scholar 

  8. V. V. Ratkin, L. N. Khetchikov, V. A. Pakhomova, and L. F. Simanenko, “Composition and physicochemical conditions of sphalerite crystallization as reflection of zoning of the Partizanskoe polymetallic deposit,” Tikhookean. Geol., No. 3, 72–82 (1994).

    Google Scholar 

  9. S. M. Rodionov, Tin Metallogeny of East Russia (Nauka, Moscow, 2005) [in Russian].

    Book  Google Scholar 

  10. L. F. Simanenko, “Modes of trace element occurrence in galena from the Partizansky base metal-skarn deposit, Primorye,” Russ. J. Pac. Geol. 26(2), 144–152 (2007).

    Article  Google Scholar 

  11. V. Yu. Chevychelov, Extended Abstract of Candidate’s Dissertation in Geology and Mineralogy (Mosk. Gos. Univ., Moscow, 1981).

    Google Scholar 

  12. M. Shimizu and N. Shikazono, “Iron and zinc partitioning between coexisting stannite and sphalerite: a possible indicator of temperature and sulfur fugacity,” Mineral. Deposita 20(4), 314–320 (1985).

    Article  Google Scholar 

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Correspondence to L. F. Simanenko.

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Original Russian Text © L.F. Simanenko, V.V. Ratkin, V.A. Turchin, 2015, published in Tikhookeanskaya Geologiya, 2015, Vol. 34, No. 2, pp. 44–60.

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Simanenko, L.F., Ratkin, V.V. & Turchin, V.A. Mineral assemblages of the porphyry tin-polymetallic ores of Mount Krasnaya paleovolcano of the Krasnogorsky deposit in the Dal’negorsk ore district. Russ. J. of Pac. Geol. 9, 120–135 (2015). https://doi.org/10.1134/S1819714015020062

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  • DOI: https://doi.org/10.1134/S1819714015020062

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