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The Cenozoic Era The Modern World Emerges Tectonics
Earth History GEOL 2110 The Cenozoic Era The Modern World Emerges Tectonics
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Major Concepts The volcanic null that corresponded with the Laramide Orogeny starting in the late Cretaceous ended in the late Eocene epoch (~40Ma) with the resumption of arc magmatism along the western margin of NA Starting in the Miocene (~20Ma), the collision of the East Pacific Rise created a transform boundary between the Pacific and NA plates; this brought on the Basin and Range-style extension tectonics, the uplift of the Colorado Plateau, the creation of the Rio Grande Rift, and shift in the motion of the Pacific plate The collision of India and various microcontinents spalled from Gondwana’s break-up closed the Tethy’s Sea and created the Alpine-Himalayan orogenic belt
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Summary of the Cenozoic
PEOMPP
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Early Cenozoic (66-40 Ma) Paleocene - Mid-Eocene
Laramide Orogeny Block uplift of the Precambrian basement
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Laramide Orogeny Magmatic Null Zone – Shallow Slab Subduction
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Sedimentation in Laramide Intermontane Basins
BH PR WR GR U Coal Seams in the Powder River Basin, WY Lacustrine Shales of the Green River Basin, UT Lacustrine Shales Marls Bryce Canyon NP, UT
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Middle Cenozoic (40-20 Ma) Late Eocene – Oligocene – Mid-Miocene
Resumption of continental volcanic arc magmatism as subduction of the Farallon Plate steepens Tectonics during the Oligocene (~30 Ma)
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Middle Cenozoic (40-20 Ma) San Juan Volcanic Field
La Garita Caldera (28Ma) San Luis Tuff, Wheeler Geologic Monument
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Middle Cenozoic (40-20 Ma) Burial and Exhumation of the Laramide Mountains
Laramide Mtns Exhumed 66Ma 35 Ma Laramide Mtns Re-Buried Laramide Orogeny Post- Laramide Orogeny 57 Ma Laramide Mtns Buried 15 Ma Laramide Mtns Re-Exhumed 50 Ma
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Laramide Sediments and Volcanic Ash Spreads across the Great Plains
Eocene – Oligocene fluvial sediments of the White River Group, Badlands, SD
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Late Cenozoic (20-0 Ma) Mid-Miocene – Pliocene –Pleistocene - Holocene
Mid-Miocene (~15 Ma) Pliocene (~5 Ma) Collision of East Pacific Rise with NA plate creates the San Andreas Transform Fault System, Basin and Range Province, Colorado Plateau and Rio Grand Rift
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Basin and Range Province Extensional Thinning of the Crust
Sevier Deformation Listric Normal Faults
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Basin and Range Province Extensional Thinning of the Crust
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Basin and Range Province Extensional Thinning of the Crust
Extension due to mantle upwelling in area of Slab Gap
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Basin and Range Province Extensional Thinning of the Crust
As the SA transform boundary grows, Basin and Range Extension migrates to the North. Establishment of rift zone in the Gulf of California kills extension in the southern Basin and Range.
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The Slicing and Dicing of California
Narrow fault –bound basins rapidly fill with great thickness of sediment that are simultaneously deformed (e.g., Ventura Basin) Pliocene (~5 Ma)
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Uplift of the Colorado Plateau Rejuvenation of Mature Rivers
Mantle Upwelling? Pliocene (~5 Ma)
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Columbia River Basalts, Snake River Basalts, and the Yellowstone Hotspot
Edge of Craton NA Drift Yellowstone Newberry
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Mantle Plume-Generated Volcanism
Columbia River Basalts Yellowstone Hydrothermal Field Newberry Rhyolite
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Present-Day Tectonic Picture
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Pacific Plate Tectonics
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Passive Margins East and South
Erosion of North America – River and Deltaic Deposits Triassic-sourced Halite Deposits Pangea Break-up – Shallow Marine Deposits
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Passive Margins East and South
Rejuvenation of the Appalachians
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The Closing of the Tethys Sea
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The Closing of the Tethys Sea
25 Ma The Closing of the Tethys Sea 5-6 Ma Mediteranean Dries Up -Evaporites 4 Ma Straits of Gibraltar open up
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Tectonics of East Asia
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Next Lecture The Cenozoic The Modern World Emerges Climate and Life Quiz on Chapter 15
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