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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Bibliographic Details
Main Author: Schickhoff, Amelie
Format: Master Thesis
Language:English
Published: UiT Norges arktiske universitet 2024
Subjects:
Online Access:https://hdl.handle.net/10037/34085