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Complex resistivity dipole-dipole data with a=100, n=1 to 7 were collected over the deposit using time domain as well as frequency domain methods in 1990 - 1991. Some lines were also surveyed with 50 metre dipole spacing, but these surveys were less successful at delineating the deeper, northern zone of mineralization. CRA Exploration Pty. Ltd. inverted the frequency domain results using UBC-GIF algortihms. Results from line 47000E (2km long) are presented here.
For a summary of dipole-dipole resistivity/induced polarization surveying, see chapter 6.
 home © UBC-GIF
April 23, 2007
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