minerals Article Mineralogy of Phoscorites of the Arbarastakh Complex (Republic of Sakha, Yakutia, Russia) Mikhail Nikolaevich Kruk 1,*, Anna Gennadievna Doroshkevich 1,2, Ilya Romanovich Prokopyev 1,3 and Ivan Aleksandrovich Izbrodin 1,2 1 Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, 630090 Novosibirsk, Russia;
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[email protected] (I.A.I.) 2 Geological Institute, Siberian Branch of the Russian Academy of Sciences, 670047 Ulan-Ude, Russia 3 Department of Geology and Geophysics, Novosibirsk State University, 630090 Novosibirsk, Russia * Correspondence:
[email protected]; Tel.: +7-913-981-40-34 Abstract: The Arbarastakh ultramafic carbonatite complex is located in the southwestern part of the Siberian Craton and contains ore-bearing carbonatites and phoscorites with Zr-Nb-REE mineralization. Based on the modal composition, textural features, and chemical compositions of minerals, the phoscorites from Arbarastakh can be subdivided into two groups: FOS 1 and FOS 2. FOS 1 contains the primary minerals olivine, magnetite with isomorphic Ti impurities, phlogopite replaced by tetraferriphlogopite along the rims, and apatite poorly enriched in REE. Baddeleyite predominates among the accessory minerals in FOS 1. Zirconolite enriched with REE and Nb and pyrochlore are found in smaller quantities. FOS 2 has a similar mineral composition but contains much less olivine, magnetite is enriched in Mg, and the phlogopite is enriched in Ba and Al. Of the accessory minerals, pyrochlore predominates and is enriched in Ta, Th, and U; baddeleyite is Citation: Kruk, M.N.; Doroshkevich, A.G.; Prokopyev, I.R.; Izbrodin, I.A.