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Abstract

The main objective of the Preissac-Lacorne field trip is to familiarize the participant with the important geologic and metallogenic characteristics of the Li-, Be-, Ta- and Mo-bearing granitic pegmatites and associated peraluminous monzogranite plutons. These felsic intrusives constitute the youngest magmatic events related to the emplacement of the Preissac-Lacorne batholith.

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