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Formation conditions of high-grade gold–silver ore of epithermal Tikhoe deposit, Russian Northeast

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Abstract

The Tikhoe epithermal deposit is located in the Okhotsk–Chukotka volcanic belt (OChVB) 250 km northeast of Magadan. Like other deposits belonging to the Ivan’insky volcanic–plutonic depression (VTD), the Tikhoe deposit is characterized by high-grade Au–Ag ore with an average Au grade of 23.13 gpt Au and Au/Ag ratio varying from 1: 1 to 1: 10. The detailed explored Tikhoe-1 orebody is accompanied by a thick (20 m) aureole of argillic alteration. Pyrite is predominant among ore minerals; galena, arsenopyrite, sphalerite, Ag sulfosalts, fahlore, electrum, and küstelite are less abundant. The ore is characterized by abundant Sebearing minerals. Cu–As geochemical specialization is noted for silver minerals. Elevated Se and Fe molar fractions of the main ore minerals are caused by their formation in the near-surface argillic alteration zone. The veins and veinlets of the Tikhoe-1 ore zone formed stepwise at a temperature of 230 to 105°C from Nachloride solution enriched in Mg and Ca cations with increasing salinity. The parameters of the ore-forming fluid correspond to those of epithermal low-sulfidation deposits and assume the formation of high-grade ore under a screening unit of volcanic rocks. In general, the composition of the ore-forming fluid fits the mineralogy and geochemistry of ore at this deposit. The similarity of the ore composition and parameters of the ore-forming fluid between the Tikhoe and Julietta deposits is noteworthy. Meanwhile, differences are mainly related to the lower temperature and fluid salinity at the Julietta deposit with respect to the Tikhoe deposit. The fluid at the Julietta deposit is depleted in most components compared with that at the Tikhoe deposit except for Sb, Cd, and Ag. The results testify to a different erosion level at the deposits as derivatives of the same ore-forming system. The large scale of the latter allows us to predict the discovery of new high-grade objects, including hidden mineralization, which is not exposed at the ore field flanks and beyond them.

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References

  • Bodnar, R.J. and Vityk, M.O., Interpretation of microterhrmometric data for H2O–NaCl fluid inclusions, Fluid Inclusions in Minerals: Methods and Applications, Siena: Pontignano, 1994, pp. 117–130.

    Google Scholar 

  • Borisenko, A.S., Cryometric study of salt composition of gas–liquid inclusions in minerals, Geol. Geofiz., 1977, no. 8, pp. 16–27.

    Google Scholar 

  • Bortnikov, N.S., Genkin, A.D., and Kovalenker, V.A., Mineralogical–geochemical indicators of conditions of hydrothermal ore formation, in Endogennye rudnye raiony i mestorozhdeniya (Endogenic Ore Districts and Deposits), Moscow: Nauka, 1987, p. 40.

    Google Scholar 

  • Brown, P., Flincor: a computer program for the reduction and investigation of fluid inclusion data, Am. Mineral., 1989, vol. 74, pp. 1390–1393.

    Google Scholar 

  • Danilin, M.V., Mineralogical zoning—criteria of hidden gold–silver mineralization of the Ivan’inskoe ore cluster (Magadan region’), Rudy Met., 2011, no. 3–4, pp. 54–55.

    Google Scholar 

  • Hedenquist, J.W., Arribas, A., and Gonzalez–Urien, E., Exploration for epithermal gold deposits, in Gold in 2000, SEG Shortcourse, 2000, vol. 13, pp. 245–277.

    Google Scholar 

  • Kovalenker, V.A., Structural and mineralogical–geochemical zoning of epithermal deposits as basis for the prediction assessment of deep horizons, in Sovremennye problemy geologii i razvitiya mineral’no–syr’evoi bazy Respubliki Uzbekistan (Modern Problems of Geology and Development of Raw Mineral Base of Uzbekistan Republic), Tashkent: IMR, 2007, pp. 84–86.

    Google Scholar 

  • Kovalenker, V.A. and Plotinskaya, O.Yu., Mineral assemblages of Cu–Sn–sulfides as indicators of Hs–Is transition in epithermal environment, Acta Mineral.–Petrogr., Abstr. Ser., 2010, vol. 6, p. 225.

    Google Scholar 

  • Kryazhev, S.G., Prokof’ev, V.Yu., and Vasyuta, Yu.V., Application of ICP MSin analyzing ore–forming fluid, Vestn. Mosk. Gos, Univ., Ser. Geol., 2006, no. 4, pp. 30–36.

    Google Scholar 

  • Obushkov, A.V., Struzhkov, S.F., Natalenko, M.V., et al., Geology and mineralogy of ore at the hidden Engteri Au–Ag deposit, the Magadan Region, Geol. Ore Deposits, 2010, vol. 52, no. 6, pp. 459–478.

    Article  Google Scholar 

  • Prokof’ev, V.Yu., Ali, A.A., Volkov, A.V., et al., Geochemical peculiarities of ore–forming fluid of the Juliette Au–Ag epithermal deposit (Northeastern Russia), Dokl. Earth Sci., 2015, vol. 460, no. 1, pp. 87–91.

    Article  Google Scholar 

  • Roedder, E., Fluid Inclusions. Rev. Mineral., 1984, vol. 12.

  • Ryzhov, O.B., Struzhkov, S.F., Aristov, V.V., et al., Geological structure and composition of ores of the Juliette gold–silver deposit (Northeast Russia), Rudy Met., 1995, no. 2, pp. 66–78.

    Google Scholar 

  • Savva, N.E. and Fidrya, I.L., Reflection of regional metallogenic featyres of territory in the mineralogical–geochemical specialization of ores of the Juliette gold–silver deposit, in Mineralogiya i geneticheskie osobennosti mestorozhdenii zolota i serebra (Mineralogy and Genetic Features of Gold and Silver Deposits), Magadan: SVKNII, 1996, pp. 119–130.

    Google Scholar 

  • Savva, N.E., Pal’yanova, G.A., and Byankin, M.A., The problem of genesis of gold and silver sufides and selenides in the Kupol deposit (Chikchi Peninsula, Russia), Russ Geol. Geophys., 2012, vol. 53, no. 3, pp. 457–466.

    Article  Google Scholar 

  • Sidorov, A.A., Zoloto–serebryanaya formatsiya Vostochno–Aziatskikh vulkanogennykh poyasov (Gold–Silver Formation of the East Asian Volcanogenic Belts), Magadan: SVKNII, 1978.

    Google Scholar 

  • Sidorov, A.A., Belyi, V.F., Volkov, A.V., et al., The gold–silver Okhotsk–Chukotka volcanic belt, Geol. Ore Deposits, 2009, vol. 51, no. 6, pp. 441–455.

    Article  Google Scholar 

  • Strujkov, S.F., Ryjov, O.B., Aristov, V.V., et al., Geological structure and ore mineralogy of the Julietta gold–silver deposit, Northeast Russia, Int. Geol. Rev., 1996, vol. 38, pp. 625–648.

    Article  Google Scholar 

  • Struzhkov, S.F. and Konstantinov, M.M., Metallogeniya zolota i serebra Okhotsko–Chukotskogo vulkanogennogo poyasa (Gold and Silver Metallogeny of the Okotsk–Chukotka Voclanogenic Belt), Moscow: Nauchnyi mir, 2005.

    Google Scholar 

  • Volkov, A.V., Prokof’ev, V.Yu., Savva, N.E., et al., Ore formation at the Kupol epithermal gold–silver deposit in Northeastern Russia deduced from fluid inclusion study, Geol. Ore Deposits, 2012, vol. 54, no. 4, pp. 295–303.

    Article  Google Scholar 

  • Volkov, A.V., Prokof’ev, V.Yu., Ali, A.A., et al., Peculiarities of ore formation at the N’yavlenga Au–Ag epithermal deposit, Northeast Russia, Dokl. Earth Sci., 2014, vol. 458, no. 3, pp. 10063–1066.

    Google Scholar 

  • Yuningsih, E.T., Matsueda, H., and Rosana, M.F., Epithermal gold–silver deposits in Western Java, Indonesia: gold–silver selenide–telluride mineralization, Indones. J. Geosci., 2014, vol. 1, no. 2, pp. 71–81.

    Article  Google Scholar 

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Correspondence to A. V. Volkov.

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Original Russian Text © A.V. Volkov, E.E. Kolova, N.E. Savva, A.A. Sidorov, V.Yu. Prokof’ev, A.A. Ali, 2016, published in Geologiya Rudnykh Mestorozhdenii, 2016, Vol. 58, No. 5, pp. 476–491.

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Volkov, A.V., Kolova, E.E., Savva, N.E. et al. Formation conditions of high-grade gold–silver ore of epithermal Tikhoe deposit, Russian Northeast. Geol. Ore Deposits 58, 427–441 (2016). https://doi.org/10.1134/S107570151605007X

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