Central Atlantic magmatic province

Central Atlantic magmatic province

Jesse Russell Ronald Cohn

     

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ISBN: 978-5-5149-0637-6

High Quality Content by WIKIPEDIA articles! 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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