CONCENTRIC-ZONAL AGGREGATE OF REE MINERALS IN FELDSPAR PEGMATITE OF THE VISHNEVYE MOUNTAINS, SOUTH URALS

A concentric-zonal texture of mineral aggregate observed in alkali pegmatite of the Vishnevye Mountains was formed as a result of melt-fluid crystallization in a closed system. At the first stage, rare large monazite crystals were crystallized creating wave concentration fields. Allanite-(Ce), bastn...

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Main Author: V.A. Popov
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2019-03-01
Series:Минералогия
Subjects:
Online Access:https://journal.mineralogy.ru/wp-content/uploads/2019/09/2019-1-3.pdf
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author V.A. Popov
author_facet V.A. Popov
author_sort V.A. Popov
collection DOAJ
description A concentric-zonal texture of mineral aggregate observed in alkali pegmatite of the Vishnevye Mountains was formed as a result of melt-fluid crystallization in a closed system. At the first stage, rare large monazite crystals were crystallized creating wave concentration fields. Allanite-(Ce), bastnäsite-(Ce), chevkinite-(Ce), thoroaeschinite, apatite-(CaF), zircon, calcite and other minerals crystallized in the end of the monazite growth. Feldspars (syntactic intergrowths of albite with Kfeldspar) were dominant in the final stage of crystallization. The change in the composition of meltfluid (magma) from phosphate-silicate to silicate is atypical.
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spelling doaj-art-1e5a2af592874f30bd7a8ba52d8fa8f02025-08-20T02:48:23ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442019-03-01512428CONCENTRIC-ZONAL AGGREGATE OF REE MINERALS IN FELDSPAR PEGMATITE OF THE VISHNEVYE MOUNTAINS, SOUTH URALSV.A. Popov0South Urals Federal Research Center of Mineralogy and Geoecology UB RASA concentric-zonal texture of mineral aggregate observed in alkali pegmatite of the Vishnevye Mountains was formed as a result of melt-fluid crystallization in a closed system. At the first stage, rare large monazite crystals were crystallized creating wave concentration fields. Allanite-(Ce), bastnäsite-(Ce), chevkinite-(Ce), thoroaeschinite, apatite-(CaF), zircon, calcite and other minerals crystallized in the end of the monazite growth. Feldspars (syntactic intergrowths of albite with Kfeldspar) were dominant in the final stage of crystallization. The change in the composition of meltfluid (magma) from phosphate-silicate to silicate is atypical.https://journal.mineralogy.ru/wp-content/uploads/2019/09/2019-1-3.pdfmonazite-(ce)rare metal and rare-earth mineralsalkali pegmatitesdissipative texturesvishnevye mountainssouth ural
spellingShingle V.A. Popov
CONCENTRIC-ZONAL AGGREGATE OF REE MINERALS IN FELDSPAR PEGMATITE OF THE VISHNEVYE MOUNTAINS, SOUTH URALS
Минералогия
monazite-(ce)
rare metal and rare-earth minerals
alkali pegmatites
dissipative textures
vishnevye mountains
south ural
title CONCENTRIC-ZONAL AGGREGATE OF REE MINERALS IN FELDSPAR PEGMATITE OF THE VISHNEVYE MOUNTAINS, SOUTH URALS
title_full CONCENTRIC-ZONAL AGGREGATE OF REE MINERALS IN FELDSPAR PEGMATITE OF THE VISHNEVYE MOUNTAINS, SOUTH URALS
title_fullStr CONCENTRIC-ZONAL AGGREGATE OF REE MINERALS IN FELDSPAR PEGMATITE OF THE VISHNEVYE MOUNTAINS, SOUTH URALS
title_full_unstemmed CONCENTRIC-ZONAL AGGREGATE OF REE MINERALS IN FELDSPAR PEGMATITE OF THE VISHNEVYE MOUNTAINS, SOUTH URALS
title_short CONCENTRIC-ZONAL AGGREGATE OF REE MINERALS IN FELDSPAR PEGMATITE OF THE VISHNEVYE MOUNTAINS, SOUTH URALS
title_sort concentric zonal aggregate of ree minerals in feldspar pegmatite of the vishnevye mountains south urals
topic monazite-(ce)
rare metal and rare-earth minerals
alkali pegmatites
dissipative textures
vishnevye mountains
south ural
url https://journal.mineralogy.ru/wp-content/uploads/2019/09/2019-1-3.pdf
work_keys_str_mv AT vapopov concentriczonalaggregateofreemineralsinfeldsparpegmatiteofthevishnevyemountainssouthurals