The origin and evolution of LCT pegmatites in Helgeland, northern Norway: stable isotope evidence from tourmaline (δ11B) and garnet (δ18O, ∆’17O)
The processes leading to formation of rare-element enriched granitic pegmatites are controversially debated amongst petrologists and economic geologists. Two contrasting genetic models discuss the necessity of a parental granitic pluton as the magma source versus an anatectic origin via partial melt...
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Format: | Master Thesis |
Language: | English |
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UiT Norges arktiske universitet
2024
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Online Access: | https://hdl.handle.net/10037/34085 |