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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
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The Koppen-Wegener maps showing continental aggregates and climatic data throughout geological time, though clever, are open to serious criticism. If the continents could drift apart in geologically late time why did they not break up in earlier eras during greater diastrophic revolutions? Geologists should not forget the principle of isostasy.
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