RARE EARTH MINERALS IN ALKALINE AND SUBALKALINE ROCKS OF THE BALBUK COMPLEX (SOUTH URALS)

Mineral composition of alkaline and subalkaline rocks of the Balbuk complex (South Urals) is characterized. The major REE minerals are monazite-(Ce), allanite-(Ce), and rhabdophane-(Ce). The highest REE content with dominant Ce, La, Nd, and Pr oxides is typical of epidote (up to 15.6 wt. %). The REE...

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Main Authors: E.P. Makagonov, V.A. Kotlyarov
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2016-06-01
Series:Минералогия
Subjects:
Online Access:https://journal.mineralogy.ru/wp-content/uploads/2019/09/2016-2-4.pdf
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author E.P. Makagonov
V.A. Kotlyarov
author_facet E.P. Makagonov
V.A. Kotlyarov
author_sort E.P. Makagonov
collection DOAJ
description Mineral composition of alkaline and subalkaline rocks of the Balbuk complex (South Urals) is characterized. The major REE minerals are monazite-(Ce), allanite-(Ce), and rhabdophane-(Ce). The highest REE content with dominant Ce, La, Nd, and Pr oxides is typical of epidote (up to 15.6 wt. %). The REE-bearing epidote crystallized at the last stage of formation of alkaline-subalkaline rocks and at the initial stage of formation of skarns. Rhabdophane-(Ce) is a product of decomposition of REE-bearing epidote during metasomatic processes. The rocks of the Balbuk complex are the primary sources of REEs for amfibole and chlorite rocks, which are developed after alkaline and subalkaline rocks, as well as for weathered rocks.
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spelling doaj.art-b2086eba75ff4888bce059b8cbb57be62025-03-10T08:11:44ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442016-06-01223443RARE EARTH MINERALS IN ALKALINE AND SUBALKALINE ROCKS OF THE BALBUK COMPLEX (SOUTH URALS)E.P. Makagonov0V.A. Kotlyarov1Institute of Mineralogy UB RASInstitute of Mineralogy UB RASMineral composition of alkaline and subalkaline rocks of the Balbuk complex (South Urals) is characterized. The major REE minerals are monazite-(Ce), allanite-(Ce), and rhabdophane-(Ce). The highest REE content with dominant Ce, La, Nd, and Pr oxides is typical of epidote (up to 15.6 wt. %). The REE-bearing epidote crystallized at the last stage of formation of alkaline-subalkaline rocks and at the initial stage of formation of skarns. Rhabdophane-(Ce) is a product of decomposition of REE-bearing epidote during metasomatic processes. The rocks of the Balbuk complex are the primary sources of REEs for amfibole and chlorite rocks, which are developed after alkaline and subalkaline rocks, as well as for weathered rocks.https://journal.mineralogy.ru/wp-content/uploads/2019/09/2016-2-4.pdfree mineralssubalkaline rocksbalbuk complexsouth urals
spellingShingle E.P. Makagonov
V.A. Kotlyarov
RARE EARTH MINERALS IN ALKALINE AND SUBALKALINE ROCKS OF THE BALBUK COMPLEX (SOUTH URALS)
Минералогия
ree minerals
subalkaline rocks
balbuk complex
south urals
title RARE EARTH MINERALS IN ALKALINE AND SUBALKALINE ROCKS OF THE BALBUK COMPLEX (SOUTH URALS)
title_full RARE EARTH MINERALS IN ALKALINE AND SUBALKALINE ROCKS OF THE BALBUK COMPLEX (SOUTH URALS)
title_fullStr RARE EARTH MINERALS IN ALKALINE AND SUBALKALINE ROCKS OF THE BALBUK COMPLEX (SOUTH URALS)
title_full_unstemmed RARE EARTH MINERALS IN ALKALINE AND SUBALKALINE ROCKS OF THE BALBUK COMPLEX (SOUTH URALS)
title_short RARE EARTH MINERALS IN ALKALINE AND SUBALKALINE ROCKS OF THE BALBUK COMPLEX (SOUTH URALS)
title_sort rare earth minerals in alkaline and subalkaline rocks of the balbuk complex south urals
topic ree minerals
subalkaline rocks
balbuk complex
south urals
url https://journal.mineralogy.ru/wp-content/uploads/2019/09/2016-2-4.pdf
work_keys_str_mv AT epmakagonov rareearthmineralsinalkalineandsubalkalinerocksofthebalbukcomplexsouthurals
AT vakotlyarov rareearthmineralsinalkalineandsubalkalinerocksofthebalbukcomplexsouthurals