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Examples
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The contact zone between metasedimentary and tonalitic rocks has now become a target for high-grade mineralization, possibly with more silver and base-metal rich zones as indicated in hole 11I-4.
unknown title 2011
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Drilling and mapping show that the gold veins exist within a WNW package of tonalitic rocks sandwiched between metasedimentary rocks to the SW and higher grade gneiss to the NE with stresses creating strong E-W shear veins as the Main and Deep Trench and minor NE tensional vein-faults.
unknown title 2011
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