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

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 (...

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Bibliographic Details
Main Authors: V. I. Popova, M. A. Rassomahin, V. A. Kotlyarov
Format: Article
Language:English
Published: A.N. Zavaritsky Institute of Geology and Geochemistry 2016-08-01
Series:Литосфера
Subjects:
Online Access:https://www.lithosphere.ru/jour/article/view/37
Description
Summary: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.
ISSN:1681-9004
2500-302X