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Post Info TOPIC: Central Atlantic Magmatic Province
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Central Atlantic Magmatic Province
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The Central Atlantic magmatic province (CAMP) is a large connected magma flow formed during the breakup of Pangaea during the Mesozoic Era. The initial breakup of Pangaea in early Jurassic time provided a legacy of basaltic dikes, sills, and lavas over a vast area around the present central North Atlantic Ocean.
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