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Part 4: Uncommon Magmatic Structures in Granites of the Borborema ProvinceRoberto Weinberg, Monash University, Australia |
Magmatic Structures Continued
A) Squeezed and bent cumulate K-feldspar. Is this magmatic?
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B) Tail in K-feldpar megacryst (5 cm long), accompanied by other grains with no tails.
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C) Solid-state zoned K-feldspar from Pedra Mijada Pluton for comparison
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