Szczegóły publikacji
Opis bibliograficzny
Brucyt z kopalni serpentynitu w Nasławicach k. Sobótki — Brucite from the serpentinite quarry at Nasławice near Sobótka, Lower Silesia, Poland / Wiesław HEFLIK, Magdalena DUMAŃSKA-SŁOWIK, Mirosław Kotowski // Przegląd Geologiczny ; ISSN 0033-2151 . — 2026 — vol. 74 nr 2, s. 112–116. — Bibliogr. s. 116, Abstr.
Autorzy (3)
- AGHHeflik Wiesław
- AGHDumańska-Słowik Magdalena
- Kotowski Mirosław
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 166819 |
|---|---|
| Data dodania do BaDAP | 2026-04-01 |
| Tekst źródłowy | URL |
| DOI | 10.7306/2026.9 |
| Rok publikacji | 2026 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | Przegląd Geologiczny |
Abstract
This study describes the abundant occurrence of brucite in the serpentinite quarry at Nasławice near Sobótka, Lower Silesia. The mineral appears mainly as fibrous crystals, resembling asbestos. Raman micro-spectroscopy, X-ray powder diffraction (PXRD) and X-ray fluorescence (XRF) analyses confirmed that the fibrous aggregates are composed of brucite (known as nemalite), enriched in iron. Brucite is accompanied by minor amounts of hydrotalcite, calcite and serpentine-group minerals. The formation of brucite is associated with low-temperature hydrothermal and supergene processes, including serpentinitization and dolerite alteration. The Nasławice serpentinite mine currently represents the largest known brucite occurrence in Poland, although it has no economic significance.
