Szczegóły publikacji
Opis bibliograficzny
Evolution of mariupolite (nepheline syenite) in the alkaline Oktiabrski Massif (Ukraine) as the host of potential Nb-Zr-REE mineralization / Magdalena DUMAŃSKA-SŁOWIK // Ore Geology Reviews ; ISSN 0169-1368. — 2016 — vol. 78, s. 1–13. — Bibliogr. s. 12–13, Abstr. — Publikacja dostępna online od: 2016-03-23
Autor
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 99992 |
|---|---|
| Data dodania do BaDAP | 2016-09-19 |
| Tekst źródłowy | URL |
| DOI | 10.1016/j.oregeorev.2016.03.011 |
| Rok publikacji | 2016 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Czasopismo/seria | Ore Geology Reviews |
Abstract
Mariupolite, aegirine-albite nepheline syenite, outcropping only in the Oktiabrski massif in south-eastern Ukraine, is a potential resource of Nb, Zr and REE for future exploration and development. Some types of this rock can be also used in ceramics, glass and building industry and jewellery. Mariupolite is composed of (1) magmatic and (2) subsolidus and hydrothermal components. The magmatic assemblage includes zircon, aegirine, nepheline, albite, K-feldspar, pyrochlore, fluorapatite, fluorbritholite-(Ce) and magnetite. Alkaline-carbonate-chloride-rich fluids exsolved very early in the history of the rock, in a late stage of, or directly after, its consolidation, induced intensive high-temperature alteration of the primary mariupolite components resulted in formation of cancrinite, calcite, fluorite, REE-bearing minerals such as monazite, parasite-(Ce), bastnasite-(Ce), as well as sodalite, natrolite and hematite. The genesis of this peculiar mineralization seems to be associated with multistage magmatic and tectonic activity of the Ukrainian Shield and fluids mediated metasomatic processes.
