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Figure 7B. Chondrite-normalized REE patterns for rhyolites
C and X, and the quartz-feldspar porphyry at the Fetais deposit. Rhyolites
C and X have patterns comparable to those of rhyolites A and B, whereas
the quartz-feldspar porphyry shows depletion in the heavy REE (more
calc-alkaline). |
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