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(1987), Gold Deposits of Western Australia, BMR Datafile (MINDEP), Resource Deposit 3, Department of Primary Industries and Energy/ Bureau of Mineral Resources Geology and Geophysics, Commonwealth Government of Australia, 1987mock, C. (2003) The Mount Percy Gold Deposit Kalgoorlie Western Australia, CRC LEME 2003 ; Butt, C.

Percy Gold Deposit Area Western Australia, CRC LEME 2003Hollis, S.

Common colour of the mineral is pale green to emerald green depending on the amount of Cr substitution.

The micaceous crystals are flexible and slightly sectile with a hardness of 2-2.5 on the Mohs scale.

Fuchsite's radioactivity due to its potassium (K) content is barely detectable.

(1992), Archaean Gold Mineralisation in a Normal Motion Shear Zone at Harbour Lights Leonora Western Australia, Mineralium Deposita, Vol 27 (3), pp 182-191, June 1992. (2014), Contrasting Structural Styles of Gold Deposits in the Leonora Domain, Australian Journal of Earth Sciences, Vol 61 (7) pp 881-917, 2014 ; Duuring, P., Hagemann, S.

Hydrothermal alteration, ore fluid characteristics, and gold depositional processes along a trondhjemite-komatiite contact at Tarmoola, Western Australia.

Trivalent chromium replaces one of the aluminium (Al) atoms in the general muscovite formula producing the apple green hue distinctive of fuchsite.

It is often found in minute micaceous aggregates (with individual plates barely visible), as a major component of chromium rich phyllitic or schistose metamorphic rocks of the greenschist facies.

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