Abstract
Rare minerals represented by oxides, fluorides, F-carbonates and REE arsenates in association with monazite-Ce, monazite-Th, xenotime-Y and zonal REE fluorite were identified in the rare-metal ores of the Sn–W deposits of Lesser Khingan, Amur region. Rare lanthanide minerals are described, including fluocerite, bastnaesite, and gasparite-Ce, which was found for the first time in Russia in the Sn–W greisens, and chernovite-Y, the second find in the greisens of the Russian Far East. The influence of arsenic fluids at the late hydrothermal stage caused the replacement of xenotime-Y and monazite-Ce by diverse REE minerals with different lanthanide proportions. It is found that these minerals differ in chemical composition from the same minerals described in other deposits elsewhere. Due to the variable valence state of arsenic and the complete isomorphism between rare earths, arsenates can be used as indicators of redox conditions of their deposition.
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REFERENCES
V. I. Alekseev and Yu. B. Marin, “Chernovite-(Y) and other arsenic minerals in the rare-metal granites and greisens of Far East,” Zap. Ross. Mineral. O-va, No. 6, 118–125 (2012).
D. K. Voznyak, V. M. Bel’s’kii, O.A. Vishnevs’kii, K. O. l’chenko, S. Kurilo, “Oxyfluocerite-(Se) of the Volhynia camera pegmatites (Ukrainian Shield),” Mineral. Zh., No. 1, 3–16 (2017).
B. A. Goldin, N. P. Yushkin, and M. V. Fishman, “New yttrium mineral—chernovite,” Zap. Vsesoyuz. Mineral. O-va, 2nd Series, 96 (6), 699–704 (1967).
V. G. Gonevchuk, B. I. Semenyak, and P. G. Korostelev, “Khingan—Okhotsk metallogenic belt in the terrane concept,” Ore Deposits of Continental Margins (Dal’nauka, Vladivostok, 2000), Vol. 1, pp. 35–54 [in Russian].
D. P. Grigor’ev, “Probable relation of ionic and covalent bonds of arsenic in different minerals and variability of bonds in mineral formation,” Problems of Geochemistry (Nauka, Moscow, 1965), pp. 449–462 [in Russian].
A. V. Dubinin, Rare-Earth Element Geochemistry in Ocean (Nauka, Moscow, 2006) [in Russian].
P. G. Korostelev, S. B. Demashov, A. M. Kokorin, D. K. Kokorina, and E. Ya. Sinyakov, “Topaz greisens of the Khingan deposit,” Tikhookean. Geol., No. 5, 117–125 (1994).
P. G. Korostelev, B. I. Semenyak, S. B. Demashov, A. M. Kokorin, D. K. Kokorina, A. P. Nedashkovskii, and E. Ya. Sinyakov, “Peculiarities of ores of the deposits of the Khingan—Olonoi district,” Ore Deposits of Continental Margins (Dal’nauka, Vladivostok, 2000), Vol. 1, pp. 202–225 [in Russian].
O. A. Krasil’shchikova, A. N. Tarashchan, and A. N. Platonov, Color and Luminescence of Natural Fluorite (Naukova dumka, Kiev, 1986) [in Russian].
V. V. Lyakhovich and V. I. Noneshnikova, Accessory Minerals of the Western Tuva Granite Intrusions and Related Vein Rocks (IMGRE AN SSSR, Moscow, 1961).
V. V. Moroshkin and V. A. Rassulov, “X-ray luminescence of fluorite from deposits of different formation-genetic types,” Zap. Ross. Mineral. O-va 31 (4), 59–70 (2002).
I. V. Pekov, A. N. Alimova, N. N. Kononkova, and A. A. Kanonerov, “Mineralogy of the Mochalin Log at the Southern Urals,” Ural’sk. Geol. Zh. 4 (28), 127–144 (2002).
V. I. Silaev, V. N. Filippov, A. F. Khazov, A. B. Makeev, and P. P. Yukhtanov, “Chernovite system: a new view through a half of century after discovery of the mineral,” Izv. Komi Nauchn. Ts Ural’sk. Otd. Ross. Akad. Nauk. Earth Sciences 1 (41), 69–79 (2020).
M. B. Chistyakova and M. E. Kazakova, “Fluocerite from Kazakhstan,” Tr. Fersman Minera. Muz. 19, 236–238 (1969).
L. G. Fel’dman, B. K. Surkov, and T. I. Stolyarova, “Fluocerite from rare-metal granites of the Northern Tien-Shan and some data on genetic mineralogy of REE fluorides,” Tr. Fersman Minera. Muz. 22, 143–158 (1973).
P. P. Feofilov, “Polarized luminescence of cubic crystals,” UFN 58 (1), 69–84 (1956).
О.D. Allen and W. J. Comstock, “Bastnasite and tysonite from Colorado,” Am. J. Sci. Ill. 19, 390 (1880).
T. Armbruster, C. Buhler, S. Graeser, H. A. Stalder, and G. Amthauer, “Cervadonite-(Ce), a new alpine fissure mineral,” Schweizeriche Min. Pet. Mitteilungenen 68, 125–132 (1988).
A. Brahi, F. M. Mongi, and H. Amor, “Cerium Arsenate, CeAsO4,” Acta Cryst. E 58, 98–99 (2002).
K. Breiter, R. Corjakova, and R. Skoda, “The involvement of F, CO2 and As in the alteration of Zr–Th–REE-bearing accessory minerals the Hora State Kateriny A-type granite, Chech Republic,” Can. Mineral. 47, 1375–1398 (2009).
R. Cabella, G. Lucchetti, and P. Marescotti, “Occurrence of REE arsenates from Fe–Mn Deposit. Ligurian Brianconnais domain. Maritime Alps, Italy,” Can. Mineral. 37, 961–972 (1999).
H.-J. Förster, M. Ondrejka, and P. Uher, “Mineralogical responses to subsolidus alteration of granitic rocks by oxidizing as-bearing fluids: REE arsenates and As-rich silicates from the Zinnwald granite, Eastern Erzgebirge, Germany,” Can. Mineral. 49, 913–930 (2011).
S. Graeser and H. Scwander, “Gasparite-(Ce) and Monazite-(Nd): two new minerals to the monazite group from the Alps,” Schweiz. Mineral. Petrogr. Mitt. 67, 103–113 (1987).
S. Mills, P. M. Kartashov, A. R. Kampf, and M. Raudsepp, “Arsenoflorencite-(La), a new mineral from the Komi Republic, Russian Federation: description and crystal structure,” Eur. J. Mineral. 22, 613–621 (2010).
G. V. Moralev, A. V. Borisov, S. V. Surenkov, S. P. Nagaaeva, M. B. Tarbaev, S. K. Kuznetsov, S. A. Onishenko, L. I. Epifanova, and A. A. Soboleva, “Distribution and speciation of REE at the Chudnoe and Nesterovskoe occurences of Au–Pd–REE ore mineralization in the Maldnyrd Range, Nether-Polar Urals,” Geochem. Int. 43 (11), 1078—1097 (2005).
M. Ondrejka, P. Uher, J. Pršek, and D. Ozdín, “Arsenian monazite-(Ce) and xenotime-(Y). REE arsenates and carbonates from the Tisovec–Rejkovo Rhyolite, Western Carpathians, Slovakia: composition and substitutions in the (REE,Y)XO4 System (X = P, As, Si, Nb, S),” Lithos 95, 116–129 (2007).
J. G. D. Steyn, “Tysonite from Mutue tides,” Geol. Surv. Repts. S. Africa. Bull. 35 (1961).
O. S. Vereshchagin, N. Britvin, E. N. Perova, A. I. Brusnitsyn, Y. S. Polekhovsky, V. V. Shilovskikh, V. N. Bocharov, Ate van der Burgt, S. Cuchet, and N. Meisser, “Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni Glacier, Switzerland,” Am. Mineral. 104, 1469–1480 (2019).
ACKNOWLEDGMENTS
We are grateful to the Academician N.S. Bortnikov for useful discussion of isomorphism of REE minerals and valuable advices during manuscript preparation. We are grateful to reviewers for careful reviewing of our work and valuable comments.
Funding
This work was made in the framework of the government-financed project of the Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences “Structural-Chemical Heterogeneities and Paragenetic Mineral Assemblages as Reflection of Rock and Ore genesis” no. 121041500220-0. XRF and EPMA studies were carried out at the Analytica Center for Collective Use of the Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences.
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This paper is dedicated to the memory of Pavel G. Korostelev, a great expert in and enthusiastic researcher of tin deposits in the Russian Far East
Recommended for publishing by N.A. Goryachev
Translated by M. Bogina
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Gorelikova, N.V., Semenyak, B.I., Korostelev, P.G. et al. Rare Earth Minerals in the Rare-Metal Greisens of the Verkhnee Deposit in the Khingan–Olonoisky District of the Amur Region, Russia. Russ. J. of Pac. Geol. 16, 608–623 (2022). https://doi.org/10.1134/S1819714022060033
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DOI: https://doi.org/10.1134/S1819714022060033