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Earth History GEOL 2110. The Mesozoic Era Tectonic and Geologic History o f North America. Major Concepts. The geologic history of North America during the Mesozoic Era was dominated by two contrasting tectonic processes :
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Earth History GEOL 2110 The Mesozoic Era Tectonic and Geologic History of North America
Major Concepts • The geologic history of North America during the Mesozoic Era was dominated by two contrasting tectonic processes : On the east, continental rift of Pangea was creating the present-day Atlantic margin On the west, compressional tectonics accreted exotic terranes in the early Mesozoic (Triassic and early Jurassic periods) and then became Andean-type volcanic arc in the mid- to late Mesozoic (Jurassic and Cretaceous periods). • Sedimentation in the Mesozoic was largely in western NA and was dominantly non-marine with sediment supplied by the erosion of the Appalachians and the emerging Cordilleran Orogen. • A major transgression in the Cretaceous created a Great Interior Seaway where great accumulation of marine and non-marine sediment were deposited in the Great Plains
Un-Making PangeaSuperplume disassembles the Supercontinent Late Triassic (215Ma) Now Pangea Late Cretaceous (95Ma)
Continental RiftingRift grabens and aulocogens bounded by normal faults
Mesozoic Rift Basins Non-marine-type Marine-type
Triassic Red-bed Sedimentation in the West Painted Desert Upper Triassic Chinle Formation 2013 SEG Field Trip Petrified Forest
Petrified WoodReplacement by Silica That the wood does not rot, indicates reducing environments with rapid deposition (floodplains, lagoons, ). The petrifaction process preserves the original cellular structure of the wood Groundwater picks up silica from sediment that is rich in siliceous volcanic ash that is altered to clay (bentonite)
Early Jurassic RegressionEolian SS Mark the End of the Absaroka Sequence Navajo Desert Navajo Sandstone Canyon de Chelley 2013 SEG Field Trip Canyon de Chelley
Dinos on the Dunes Dilophosaurus Coprolite?? Dino-pie Dilophosaurus Footprints in the JursassicKayenta Formation near Tuba City, AZ
Morrison FormationUpper Jurassic Dinosaur Graveyard Non-marine mudstone, sandstone, siltstone and limestone that is variegated light grey, greenish gray, or red; represents floodplains deposits Zuni Sequence Transgressive Regressive Unconformity Absaroka Sequence near Green River, UT Dinosaur National Monument, CO
Zuni Sequence Clastic Wedge Deposit in the Foreland Basin of the Cordilleran Orogen.
Next Lecture • Tectonic History of the North American Cordilleran • Quiz on Chapter 14 • (p. 351-381)