Abstract—
Scheelite of the Kekura gold deposit in the Western Chukchi Peninsula is reported for the first time. Three generations of the mineral have been identified. According to the LA–ICPMS data, the Mo content in scheelite does not exceed 0.2 ppm and the total REE ranges from 20 to 150 ppm. The REE distribution patterns of all three scheelite generations have a strong positive Eu anomaly (Eu/Eu* = 4.4–55.6), which is typical of scheelite from intrusion-related and orogenic gold deposits. The high Sr concentration (1300–12 000 ppm) is characteristic of the hypabyssal intrusion-related Au deposits. According to the fluid inclusion data, the minimal crystallization temperature of scheelite and associated quartz is 200–250°С.
Similar content being viewed by others
REFERENCES
Van Achterbergh, E., Ryan, C.G., Jackson, S.E., et al., Data reduction software for LA–ICP–MS: appendix, in Laser Ablation-ICP-Mass Spectrometry in the Earth Sciences: Principles and Applications, Sylvester, P.J., Ed., Min. Assoc. Canada, Ottawa, Ontario, Canada, 2001, vol. 29, pp. 239–243.
Baksheev, I.A., Prokof’ev, V.Yu., and Ustinov, V.I., Genesis of metasomatic rocks and mineralized veins at the Berezovskoe deposit, Central Urals: evidence from fluid inclusions and stable isotopes, Geochem. Int., 2001, vol. 39, no. 2, pp. S129–S144.
Bortnikov, N.S., Gamyanin, G.N., Vikentieva, O.V., et al., Fluid composition and origin in the hydrothermal system of the Nezhdaninsky gold deposit, Sakha (Yakutia), Russia, Geol. Ore Deposits, 2007, vol. 49, no. 2, pp. 87–128.
Brugger, J., Bettiol, A.A., Costa, S., et al., Mapping REE distribution in scheelite using luminescence, Mineral. Mag., 2000, vol. 64, no. 5, pp. 891–903.
Dostal, J., Kontak, D.J., and Chatterjee, A.K., Trace element geochemistry of scheelite and rutile from metaturbidite-hosted quartz vein gold deposits, Meguma Terrane, Nova Scotia, Canada: genetic implications, Mineral. Petrol., 2009, vol. 97, pp. 95–109.
Fu, Y., Sun, X., Zhou, H., et al., In-situ LA–ICP–MS trace elements analysis of scheelites from the giant Beiya gold-polymetallic deposit in Yunnan Province, Southwest China and its metallogenic implications, Ore Geol. Rev., 2017, vol. 80, pp. 828–837.
Ghaderi, M., Palin, J.M., Campbell, I.H., et al., Rare earth element systematics in scheelite from hydrothermal gold deposits in the Kalgoorlie–Norseman region, Western Australia, Econ. Geol., 1999, vol. 94, no. 3, pp. 423–437.
Hodgson, C.J., The structure of shear-related, vein-type gold deposits: A review, Ore Geol. Rev., 1989, vol. 4, no. 3, pp. 231–273.
Jochum, K.P., Nohl, U., Herwig, K., et al., GeoReM: A new geochemical database for reference materials and isotopic standards, Geostand. Geoanal. Res., 2005, vol. 29, no. 3, pp. 333–338.
Kempe, U. and Oberthür, Th., Physical and geochemical characteristics of scheelite from gold deposits. A reconnaissance study, in Proc. IV Biennial SGA Meeting. Turku, Finland, Rootterdam: Balkema, 1997.
Mao, J., Konopelko, D., Seltmann, R., et al., Postcollisional age of the Kumtor gold deposit and timing of Hercynian events in the Tien Shan, Kyrgyzstan, Econ. Geol., 2004, vol. 99, no. 8, pp. 1771–1780.
Martin, R.D., Syenite-Hosted Gold Mineralization and Hydrothermal Alteration at the Young Davidson Deposit, Matachewan, Ontario: Univ. Waterloo, Ontario, Canada, 2012. https://uwspace.uwaterloo.ca/bitstream/handle/ 10012/6677/Martin_Ryan.pdf. Cited April 26, 2019.
Poulin, R.S., Kontak, D.J., McDonald, A., et al., Assessing scheelite as an ore-deposit discriminator using its trace-element and REE chemistry, Can. Mineral., 2018, vol. 56, no. 3, pp. 265–302.
Ribeiro-Rodrigues, L.C., de Oliveira, C.G., and Friedrich, G., The Archean BIF-hosted Cuiaba gold deposit, Quadrilatero Ferrifero, Minas Gerais, Brazil, Ore. Geol. Rev., 2007, vol. 32, nos. 3–4, pp. 543–570.
Roberts, S., Palmer, M.R., and Waller, L., Sm–Nd and REE characteristics of tourmaline and scheelite from the Bjorkdal gold deposit, northern Sweden: evidence of an intrusion-related gold deposit, Econ. Geol., 2006, vol. 101, pp. 1415–1425.
Sciuba, M., Beaudoin, G., and Hout, F., Texture, cathodoluminescence and trace elements composition of scheelite, indicator of orogenic gold deposits, in Proc. 14th Technol. Forum, Val D’Or, Canada, 2016. http://www.consorem.ca/ presentation_pub/forum_techno_2016/presentations_ forumt_016/13H50_SCIUBA_DIVEX_2016.pdf. Cited May 6, 2019.
Song, G., Qin, K., Li, G., et al., Scheelite elemental and isotopic signatures: Implications for the genesis of skarn-type W–Mo deposits in the Chizhou area, Anhui Province, eastern China, Am. Mineral., 2014, vol. 99, nos. 2–3, pp. 303–317.
Spiridonov, E.M., The inversion plutonogenic gold–quartz associations in the Caledonides of Northern Kazakhstan, Geol. Rudn. Mestor., 1995, vol. 37, no. 3, pp. 179–207.
Spiridonov, E.M., Sokolova, N.F., Naz’mova, G.N., et al., Typical chemistry of scheelite from depth variable plutonogenic hydrothermal gold deposits, Dokl. Earth Sci., 1999, vol. 364, no. 1, pp. 47–49.
Sun, K. and Chen, B., Trace elements and Sr–Nd isotopes of scheelite: implications for the W-Cu-Mo polymetallic mineralization of the Shimensi deposit, South China, Am. Mineral., 2017, vol. 102, pp. 1114–1128.
Sun, S.S. and McDonough, W.F., Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes, in Magmatism in the Ocean Basins. Geol. Soc. London. Spec. Publ., Saunders, A.D. and Norry, M.J., Eds., 1989, vol. 42, no. 1, pp. 313–345.
Sun, X., Zhang, Y., Xiong, D., et al., Crust and mantle contributions to gold-forming process at the Daping deposit, Ailaoshan gold belt, Yunnan, China, Ore Geol. Rev., 2009, vol. 36, pp. 235–249.
Tikhomirov, P.L., Prokof’ev, V.Yu., Kal’ko, I.A., et al., Post-collisional magmatism of western Chukotka and Early Cretaceous tectonic rearrangement in northeastern Asia, Geotectonics, 2017, vol. 51, no. 2, pp. 131–151.
Tshibubudze, A., Integrated strato-tectonic, U–Pb geochronology and metallogenic studies of the Oudalan-Gorouol volcano-sedimentary Belt (OGB) and the Gorom-Gorom granitoid terrane (GGGT), Burkina Faso and Niger, West Africa, PhD Thesis, Univ. Wittwatersrand, Johannesburg, 2015. http://www.tectonique.net/waxi_theses/2015_Tshibubudze.pdf. Cited April 27, 2019.
Vikentieva, O.V., REE distribution in scheelite of gold–ore deposits, in Tez. Godich. sobr. RMO (Trans. Annu. Meet. Russ. Miner. Soc.), St. Petersburg, 2006, pp. 123–124.
Zhu, Y.-N. and Peng, J.-T., Infrared microthermometric and noble gas isotope study of fluid inclusions in ore minerals at the Woxi orogenic Au–Sb–W deposit, western Hunan, South China, Ore Geol. Rev., 2015, vol. 65, pp. 55–69.
ACKNOWLEDGMENTS
We are grateful to O.V. Vikentieva (Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences) and V.V. Smolensky (St. Petersburg Mining University) for their valuable comments, which improved the manuscript. We thank the geologists of ZAO Bazovye Metally for the samples that were kindly placed at our disposal.
Funding
This study was supported by the Russian Foundation for Basic Researches (project no. 18-35-20034).
Author information
Authors and Affiliations
Corresponding author
Additional information
Translated by I. Baksheev
About this article
Cite this article
Nagornaya, E.V., Baksheev, I.A., Anosova, M.O. et al. Scheelite of the Kekura Gold Deposit, Western Chukchi Peninsula: Trace Elements and Fluid Inclusions. Moscow Univ. Geol. Bull. 75, 159–167 (2020). https://doi.org/10.3103/S0145875220020052
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.3103/S0145875220020052