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Latest Information January 31, 1999 One hole had been completed to test a Dipole-Dipole IP anomaly located at 150 m depth. The area showed mafic and felsic volcanic outcrops on surface. This turned out to be a ``skim'' of volcanics and the hole intersected a sedimentary section with 3-6% pyrite, explaining the IP anomaly. January 31, 1999 One hole had been completed to test a Dipole-Dipole IP anomaly located at 150 m depth. The area showed mafic and felsic volcanic outcrops on surface. This turned out to be a ``skim'' of volcanics and the hole intersected a sedimentary section with 3-6% pyrite, explaining the IP anomaly. |
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