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Spodumene Pegmatites in Leinster Granite by fre is a document available to read on EtoBox.

The document discusses spodumene pegmatites associated with the Leinster Granite in southeast Ireland. It uses geochemical modeling of whole-rock samples from drill cores to investigate whether the pegmatites formed from fractional crystallization of the granite magma or partial melting of a rare-earth rich source. The results indicate the pegmatite and granite magmas likely originated from separate events and different source rocks.

Author
fre
Language
EN