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Native tungsten from the Bol'shaya Pol'ya river valley and Mt Neroyka, Russia

Published online by Cambridge University Press:  26 January 2021

Stuart J. Mills*
Affiliation:
Geosciences, Museums Victoria, GPO Box 666, Melbourne3001, Victoria, Australia
Pavel M. Kartashov
Affiliation:
Institute of Geology Ore Deposits, Petrography, Mineralogy and Geochemistry (IGEM) of Russian Academy of Sciences, Staromonetnyi pereulok 35, 109017Moscow, Russia
Anthony R. Kampf
Affiliation:
Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California90007, USA
Mike S. Rumsey
Affiliation:
Earth Sciences Department, Natural History Museum, Cromwell Road, LondonSW7 5BD, UK
Chi Ma
Affiliation:
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California91125, USA
Chris J. Stanley
Affiliation:
Earth Sciences Department, Natural History Museum, Cromwell Road, LondonSW7 5BD, UK
John Spratt
Affiliation:
Department of Core Research Laboratories, Natural History Museum, Cromwell Road, LondonSW7 5BD, UK
George R. Rossman
Affiliation:
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California91125, USA
Margarita I. Novgorodova
Affiliation:
Fersman Mineralogical Museum, Leninskiy Prospekt 18(2), Moscow117071, Russia
*
*Author for correspondence: Stuart J. Mills, Email: smills@museum.vic.gov.au

Abstract

Native tungsten (IMA2011-004), W, is officially described as a new mineral from gold placers in the Bol'shaya Pol'ya river valley, Prepolar Urals, Russia, associated with yttriaite-(Y) and from quartz veins in the Mt Neroyka rock-crystal field, Ust–Puiva, Tyumenskaya Oblast', Russia. Tungsten forms polycrystalline grains and masses, and rarely cubo-octahedra. It is silver white to steel grey in colour, with metallic lustre and grey streak. The calculated density is 19.226 g/cm3. The Vickers hardness (VHN25) is 571.45 kg/mm2. In plane polarised light, tungsten is white with a pale-yellow tint and optically isotropic. Electron microprobe analyses of Bol'shaya Pol'ya river valley material provided W 99.27, Mo 0.06, Mn 0.04, Fe 0.01, total 99.38 wt.%. The five strongest powder X-ray diffraction lines are [dobs Å(I)(hkl)]: 2.2422(100)(110), 1.5835(25)(200), 1.2929(48)(211), 1.0010(23)(310) and 0.8457(24)(321). Tungsten is cubic, Im$\bar{3}$m, a = 3.1648(4) Å, V = 31.69(4) Å3 and Z = 2. Some additional occurrences of native tungsten and technogenic tungsten found in Nature are also described.

Type
Article – Frank Reith memorial issue
Copyright
Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of The Mineralogical Society of Great Britain and Ireland

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Footnotes

This paper is part of a thematic set in memory of Frank Reith.

Associate Editor: Daniel Atencio

References

Bai, W.J., Yang, J.S., Fang, Q.S., Yan, B.G. and Zhang, Z.M. (2001) Study on a storehouse of ultrahigh pressure mantle minerals-podiform chromite deposits. Earth Science Frontiers, 8, 111122.Google Scholar
Christy, A.G. (2015) Causes of anomalous mineralogical diversity in the Periodic Table. Mineralogical Magazine, 79, 3349.CrossRefGoogle Scholar
Craig, J.R. and Vaughan, D.J. (1981) Ore Microscopy and Ore Petrography. Wiley Science, New York, 406 pp.Google Scholar
Deshpande, V.T. and Pawar, R. (1962) X-ray determination of the thermal expansion of tungsten. Current Science, 31, 497499.Google Scholar
Dvurechenskaya, S.S. and Kryazhev, S.G. (2005) Mineralogical-geochemical features of rocks and ores at the Tabornoe deposit, the western part of the Aldan Shield. Ores and Metals, 4, 1218 [in Russian].Google Scholar
Fang, Q., Bai, W., Yang, J., Xu, X., Li, G., Shi, N., Xiong, M. and Rong, H. (2009) Qusongite (WC): a new mineral. American Mineralogist, 94, 387390.CrossRefGoogle Scholar
Glushkova, E.G. and Nikiforova, Z.S. (2014) Comparative analysis of the proximal wash off placer gold and gold from metasomatites of Tabornoe ore field (western part of Aldan shield). Zapiski RMO, 143, 6673 [in Russian].Google Scholar
Gorshkov, A.I., Titkov, S.V., Bao, Y.N., Ryabchikov, I.D. and Magazina, L.O. (2006) Microinclusions in diamonds of octahedral habit from kimberlites of Shandong Province, Eastern China. Geology of Ore Deposits, 48, 326334.CrossRefGoogle Scholar
Itoh, Y. and Ishiwata, Y. (1996) Strength properties of yttrium-oxide-dispersed tungsten alloy. JSME International Journal. Ser. A, Mechanics and Material Engineering, 39, 429434.CrossRefGoogle Scholar
Kartashov, P.M., Mokhov, A.V., Gornostaeva, T.A., Bogatikov, O.A. and Ashikhmina, N.A. (2010) Mineral phases on the fracture of a glass particle and in the fines of a Luna 24 regolith sample. Petrology, 18, 107125.CrossRefGoogle Scholar
Kvasnytsya, V.M., Pavliuk, O.V., Kvasnytsya, I.V., Vysotskyi, B.L. and Gurnenko, I.V. (2014) The finding of native tungsten microcrystals in Bilokorovychi proterozoic conglomerates of the Volyn. Reports of the National Academy of Sciences of Ukraine, 11, 8894 [in Ukrainian].Google Scholar
Lassner, E. and Schubert, W.-D. (1999) Tungsten: Properties, Chemistry, Technology of the element, alloys and chemical compounds. Kluwer Academic, New York, 416 pp.CrossRefGoogle Scholar
Lukin, A.E. (2009) On native tungsten in rocks of petroliferous complexes. Reports of the National Academy of Sciences of Ukraine, 2, 121130 [in Ukrainian with English abstract].Google Scholar
Ma, C. and Rossman, G.R. (2008) Barioperovskite, BaTiO3, a new mineral from the Benitoite Mine, California. American Mineralogist, 93, 154157.CrossRefGoogle Scholar
Mokhov, A.V., Kartashov, P.M. and Bogatikov, O.A. (2007) Moon under a Microscope. Moscow, Nauka, 128 pp. [in Russian].Google Scholar
Mills, S.J., Kartashov, P.M., Kampf, A.R., Rumsey, M.S., Ma, C., Spratt, J., Rossman, G.R. and Novgorodova, M.I. (2011a) Tungsten, IMA 2011-004. CNMNC Newsletter No. 9, August 2011, page 2539; Mineralogical Magazine, 75, 25352540.Google Scholar
Mills, S.J., Kartashov, P.M., Ma, C., Rossman, G.R., Novgorodova, M.I., Kampf, A.R. and Raudsepp, M. (2011b) Yttriaite-(Y): the natural occurrence of Y2O3 from the Bol'shaya Pol'ya River, Russian Federation. American Mineralogist, 96, 11661170.CrossRefGoogle Scholar
Mokhov, A.V., Kartashov, P.M., Gornostaeva, T.A. and Bogatikov, O.A. (2014) Mercury-bearing sulphide from Lunar regolith of Mare Fecunditatis, Bulletin of the Kamchatka Regional Organization Educational and Scientific Center, Series: Earth Sciences, v.2, 24, 160164 [in Russian].Google Scholar
Novgorodova, M.I., Nedashkovskaya, N.N., Rassdazov, A.V., Trubkin, N.V., Semenov, E.I. and Koshelev, B.L. (1995) A native wolfram with inclusions of yttrium oxide from an alluvium of Bol'shaja Pol'ja river (Prepolar Ural). Doklady RAN, 340, 681684 [in Russian].Google Scholar
Pan, Y., Zhu, R., Banerjee, S.K., Gill, J. and Williams, Q. (2000) Rock magnetic properties related to thermal treatment of siderite: behavior and interpretation. Journal of Geophysical Research: Solid Earth, 105, 783794.CrossRefGoogle Scholar
Ramdohr, P. (1969) The Ore Minerals and Their Intergrowths. 3rd ed., Pergamon Press, Oxford, UK, 1174 pp.Google Scholar
Samsonov, G.V. (editor)(1968) Handbook of the Physicochemical Properties of the Elements. IFI–Plenum, New York, USA.CrossRefGoogle Scholar
Tamana, H.S. (1994) The Mineralogy and Geochemistry of Platinum Group Minerals from Eluvial and Alluvial Deposits. Doctoral dissertation, University of Manchester, UK.Google Scholar
Trent, E.M. and Wright, P.K. (2000) Metal Cutting. Butterworth-Heinemann, Boston, USA.CrossRefGoogle Scholar
Young, B.B. and Millman, A.P. (1964) Microhardness and deformation characteristics of ore minerals. Transactions of the Institute of Mining & Metallurgy (London), 7, 437466.Google Scholar