Downhole EM is useful when exploring for massive sulphides. The 15m zone of copper mineralisation discovered to date appears to be disseminated and blebby.
Unless there is massive sulphides nearby (within 30-50m), DHEM isn't going to help. From the images of the core that I have seen - I wouldn't be holding out for nearby massive sulphides.
IP is better for defining disseminated sulphides but downhole IP doesn't exist and at 400m depth, surface IP is starting to push the limits of detection.
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