Geology to me looks like a NE plunging syncline of which SYR's ground is on the southern limb. SYR cross sections show high grade zones in schist dipping roughly northwards. No suprise then that grade drops away at shallow depth to the north. Question is then do these same high grade beds reappear on the other northern limb in TON's ground and are they still of similar grade?
don't get caught holding the bag..., page-8
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