Chemical and mineralogical characterization of elbaites from the Alto Quixaba pegmatite, Seridó province, NE Brazil
The Alto Quixaba pegmatite, Seridó region, northeastern Brazil, is a 60◦/80◦SW-trending subvertical dikediscordantly intruded into biotite schists of the Upper Neoproterozoic Seridó Formation. It has three distinctmineralogical and textural zones, besides a replacement body that cuts the...
Furkejuvvon:
| Publikašuvnnas: | Anais da Academia Brasileira de Ciências |
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| Váldodahkkit: | , , , |
| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Academia Brasileira de Ciências
2005
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| Fáttát: | |
| Liŋkkat: | https://www.redalyc.org/articulo.oa?id=32777411 |
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