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Project geology
➢ Preserved amphibolite-granulite
Cleo
facies greenstones on east side of Rebecca
Pinjin Fault
➢ Rebecca deposit sits within broad
granodiorite/gneiss pile
➢ Stratabound relative to magnetic
mafic/ultramafic intrusion, Duke
similar distance
➢ Rebecca & Duke potentially on east
limb of overturned and refolded fold
(synform?)
Duchess
➢ Basalt/amphibolite and diorite to
west (dome?)
➢ Duchess mineralised structures Duke
transect geology - in granodiorite
gneiss & fine-grained biotite rich
diorite
➢ Cleo – micro-diorite/mafic
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