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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Bibliografski detalji

Glavni autor:	V.A. Popov
Format:	Artigo
Jezik:	Inglês
Izdano:	South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2019-03-01
Serija:	Минералогия
Teme:	monazite-(ce) rare metal and rare-earth minerals alkali pegmatites dissipative textures vishnevye mountains south ural
Online pristup:	https://journal.mineralogy.ru/wp-content/uploads/2019/09/2019-1-3.pdf
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