
TY  - JOUR
A1  - Bishop, J.R. 
A1  - Lewis, R.J.G. 
T1  - Time domain spectral IP measurements from the Rosebery mine
JF  - Exploration Geophysics
JO  - Explor. Geophys.
Y1  - 1985
VL  - 16
IS  - 3
SP  - 175
EP  - 176
KW  - 
UR  - https://doi.org/10.1071/EG985175 
N2  - The Rosebery mine is a volcanogenic massive sulphide deposit located on the west coast of Tasmania. Before mining, the deposit contained in excess of 15 Mt of ore with grades averaging 18% zinc, 5.5% lead, 0.5% copper, 187 g/t silver and 3.8 g/t gold. The mine lies in a sedimentary sequence within the Cambrian Mt Read Volcanics and the sulphides occur in association with (pyrite-bearing) 'Black Shales', within altered and pyritized 'Host Rocks'. The 'Footwall Schists' are siliceous and also contain disseminated pyrite. The hanging wall 'Massive Pyroclastics' are unaltered (Fig. 1). 
ER  -

