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...
محفوظ في:
| المؤلف الرئيسي: | |
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| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
2019-03-01
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| سلاسل: | Минералогия |
| الموضوعات: | |
| الوصول للمادة أونلاين: | https://journal.mineralogy.ru/wp-content/uploads/2019/09/2019-1-3.pdf |
| الوسوم: |
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