Queensland Minerals

A Summary of Major Mineral Resources, Mines and Projects, 2nd Edition

Mineralisation Age

ORE

Comments

The mineralisation is hosted by calc-silicate gneiss of the Einasleigh Metamorphics. The mineralised zone is sheared and mylonitic and is

retrogressed to chlorite schist, mica-quartz-chlorite-schist, amphibolite gneiss and epidosite.

Primary mineralisation comprises disseminated sulphides, as well as sulphides concentrated in epidote-actinolite-quartz veins.

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