New data on mineralogy of granitic pegmatites Mt. Soroch′ya, Southern Urals

• Main Authors: V. I. Popova, M. A. Rassomahin, V. A. Kotlyarov
• Format: Article
• Language: English
• Published: A.N. Zavaritsky Institute of Geology and Geochemistry 2016-01-01
• Series: Литосфера
• Subjects: гранитные пегматиты; мусковит; шерл; циркон; рутил; “стрюверит”; ксенотим-(Y); монацит-(Ce); золото; гора Сорочья; Южный Урал; granitic pegmatites; mica; schцrl; zircon; rutile; strьverite; xenotime-(Y); monazite-(Ce); gold; Mt. Soroch’ya; South Urals
• Online Access: https://test.lithosphere.ru/jour/article/view/37
• ISSN: 1681-9004; 2500-302X

Mineralogy of granitic pegmatites of Mt. Soroch′ya near Zlatoust which ore included in the Upper Riphean metamorphic mica-garnet, staurolite-garnet, and wollastonite-sillimanite-garnet schists of the Kuvash Formation is examined. Zonal pegmatite veins 30-600 m long and 1-40 m thick are composed of (from margin to centre): 1) pegmatoic quartz-two-feldspar with muscovite and biotite; 2) graphic muscovite-quartz-two-feldspar; 3) blocky with large crystals of microcline, muscovite (up to 10 cm) and quartz in small-grained quartz-albite aggregate; and 4) quartz core zones. The composition of formerly known mica, tourmaline, zircon, rutile and first time discovered xenotime-(Y), monazite-(Ce), Ta-bearing rutile (“strьverite”), and gold is ore described.