Alnoite is a rare igneous rock type belonging to the lamprophyre family, specifically a variety of mica-rich lamprophyre. It is scientifically notable for its mineralogy, chemistry, and occurrence in alkaline igneous provinces.
🌍 Origins and Naming
- Name Origin: Named after Alnö Island, Sweden, where it was first described.
- Discovery: Identified in the late 19th century during studies of alkaline complexes.
- Type Locality: Alnö Island, Västernorrland, Sweden — famous for carbonatites and lamprophyres.
🔬 Composition and Mineralogy
- Major Minerals:
- Biotite or phlogopite (mica)
- Clinopyroxene (diopside, augite)
- Olivine (sometimes altered)
- Accessory Minerals: Apatite, magnetite, perovskite, calcite.
- Texture: Porphyritic, with large mica phenocrysts in a fine-grained groundmass.
- Chemistry: Rich in potassium and magnesium; belongs to the alkaline lamprophyres.
⚙️ Geological Occurrence
- Found in alkaline igneous complexes, often associated with carbonatites and other unusual rock types.
- Localities:
- Alnö Island, Sweden (type locality).
- Other alkaline provinces worldwide, though rare.
- Geological Context: Intrusive dikes and plugs, often linked to deep mantle-derived magmas.
📖 Scientific and Collector Significance
- Petrology: Important for understanding mantle-derived alkaline magmatism and lamprophyre diversity.
- Collectors: Rarely collected as hand specimens; valued academically for its mineralogical associations.
- Economic Note: Sometimes associated with carbonatite complexes that host rare earth elements, though alnoite itself is not an ore.
✨ Conclusion
Alnoite is a mica-rich lamprophyre, first described from Alnö Island, Sweden. It is scientifically significant for its role in alkaline igneous complexes and mantle-derived magmatism, though it remains a petrological curiosity rather than an economic resource.
In short: Alnoite = mica-rich lamprophyre, rare igneous rock, first found at Alnö Island, Sweden.
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