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15:25
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Originally posted by geospud:
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Thats awesome. Thanks! I am really getting into reading about the details. I was just reading something about the formation of the deposit. It talks about the tin coming from Devonian granitoids, which at the site are 1000 m below the surface. So, the metamorphic fluids then transport the tin upwards via these shear zones where it became hosted in the dolomite layers as cassiterite? It's also talking about siliceous ores within the Bassett fault. So it seems to me that these faults and shear zones are very important for tin transport and that it's not only the offset issues that are important. Is that your reading?
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Yes, it will tell you the full story.
(20min delay)