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Project Overview

Project Number
Project Theme
Mineral Systems

The pegmatite of this study is in a Barrovian-style terrain, localised in a major shear zone, and in or near mafic-ultramafic sequences, thus explaining many of the anomalous features in its mineralogy, texture and structure.  Exploration parameters defined are mineral geochemistry, geochemical dispersion haloes and geochemically anomalous cross-cutting mafic dykes.

Page was last reviewed 13 July 2020

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