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rapakivi
igneous rock
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occurrence in Svecofennian Orogen
- In Precambrian: Orogenic belts
…by tin-bearing crustal-melt granites, called rapakivi granites after their coarse, zoned feldspar megacrysts (that is, crystals that are significantly larger than the surrounding fine-grained matrix). The rocks in this zone probably formed as a result of mantle plume activity.
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