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The breakup of the Pangean supercontinent in the Triassic-Jurassic age left great rift basins containing an extraordinary record of the physical and biological conditions which precipitated a major extinction event at the time. These basins collectively form a rift province called the Central Atlantic Margin (CAM). Leading experts LeTourneau and Olsen present a detailed review of the rift province's geology, paleobiology, and geophysics.
Publisher: Columbia University Press
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