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Published byVergílio Domingos Camelo Modified over 6 years ago
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Tectonic Evolution of the Arctic Region Since the Ordovician
By L.A. Lawver, L.M. Gahagan, and D.A. Campbell 2000, University of Texas Institute for Geophysics July 9, 2000
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The following animation is an abbreviated version, showing reconstructions every 50 million years. The original animation shows reconstructions from 450 to 0 Ma, every 1 million years.
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Ordovician Late Caradoc ã PLATES 2000 UTIG
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Devonian Late Praghian ã PLATES 2000 UTIG
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Carboniferous Tournaisian ã PLATES 2000 UTIG
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Carboniferous Kasimovian ã PLATES 2000 UTIG
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Permian Tatarian ã PLATES 2000 UTIG
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Jurassic Early Sinemurian ã PLATES 2000 UTIG
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Jurassic Kimmeridgian ã PLATES 2000 UTIG
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Cretaceous Late Albian ã PLATES 2000 UTIG
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Paleogene Late Ypresian ã PLATES 2000 UTIG
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Quaternary ã PLATES 2000 UTIG
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We wish to thank the PLATES’ sponsors for their support: Conoco, Elf, Exxon, Norsk Hydro, and Statoil.
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For more information, contact: Lisa M
For more information, contact: Lisa M. Gahagan Institute for Geophysics University of Texas at Austin
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