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Lithologically |
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The supracrustal (greenstone) belts are lithologically diverse and include basalt, greywacke, pelite, and iron formation, along with lesser andesite, dacite, rhyolite, ultramafic rocks, conglomerate, and carbonate rocks. The property geology is proving to be considerably more complex, lithologically and structurally, than had originally been envisioned and depicted on government maps. The property geology is proving to be considerably more complex, lithologically and structurally, than had originally been envisioned and depicted on government maps. |
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