At Gonneville, **bronorite and pyroxenite rocks form the upper differentiated layer of the intrusion with the more Ni-Cu-PGE-rich serpentinite (harzburgite) lying beneath and forming the lower layer.
Recent reconnaissance air-core drilling has provided the first insight into the framework of an extensive, 12km long mafic-ultramafic intrusion, with rocks likely analogous to the western margin of Chalice Mining’s Gonneville Intrusion.
Ann: Diamond Drilling underway at Sovereign Ni-Cu-PGE Project, page-34
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