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  1. Sevier orogeny - Wikipedia

    • The Sevier Fold and Thrust Belt extends from southern California near the Mexican border to Canada. Basin and Range faults cut the older Sevier thrust faults. The Sevier orogeny was preceded by sev… See more

    Sevier Or Laramide?

    Early Sevier thrusting began well before initial Laramide deformation. However, there is evidence that suggests late Sevier faults were active during the early Laramide. … See more

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    Geologic Structures

    The Sevier orogenic belt consisted of a series of thin plates along gently dipping west thrust … See more

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    How and When

    The Sevier fold and thrust belt was active between late Jurassic (201 - 145 Mya) through Eocene (56 - 34 Mya) time. The actual age of initiation of the belt is not entirely agr… See more

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    Studies

    Transverse zones and the Uinta recess
    Parallel thrust faults and folds make up a fold-thrust belt on a regional scale. At the local scale segments of the belt are connected … See more

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    Sevier Volcanism

    Voluminous volcanism is also associated with the Sevier Orogeny. Volcanic activity can be observed at modern subduction zones, (such as along the west coast of South Ame… See more

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    Foreland Sedimentation

    As Sevier thrust faults were uplifted, thrust sheet erosion occurred; those eroded sediments were then deposited where accommodation space existed. Dynamic subsidenc… See more

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  2. The Sevier orogeny was a time of active horizontal shortening and vertical thickening of the crust, in response to the Pacific Plate subducting beneath the North American Plate. The thrust faults carried their respective thrust sheets up to 50 miles of displacement and the large folds have amplitudes of 5,000 to 10,000 feet.
    www.isu.edu/digitalgeologyidaho/fold-thrust-belt/
    The deformation took place between 165 million and 80 million years ago during the Jurassic and Cretaceous periods. It produced a zone of eastward-directed thrust faults and folds that represent 40 to 65 kilometres (25 to 40 miles) of crustal shortening in response to compressional forces.
    www.britannica.com/science/Sevier-orogeny
    Folding and thrust faulting occurred during the Cretaceous to Paleocene Sevier Orogeny (~130-60 Ma). The Sevier Orogeny was a time of active compression, in response to the Pacific Plate subducting beneath the North American Plate.
    digitalgeology.aws.cose.isu.edu/Digital_Geology_I…
    Similar styles and ages of thrust faults also occur in the Rocky Mountains of Montana, Canada, and Alaska. The process that created this stacking up and eastward pushing of thrust-fault slabs is called the Sevier orogeny, named after the Sevier River in Utah.
    commons.wvc.edu/rdawes/Lectures/lect7.html
     
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  4. Sevier-Laramide fold-thrust belt - Idaho State University

    WEBLearn about the geology and history of the fold-thrust belt of the Cretaceous Sevier-Laramide orogenic belt in Idaho and the North American Cordillera. Explore maps, cross sections, and slideshows of …

     
  5. Fault Slip and Exhumation History of the Willard …

    WEBJul 18, 2019 — What were the ages for onset and cessation of fault slip in the western part of the Sevier fold-thrust belt at the latitude of northern Utah, and did slip rates vary temporally? What were the connections …

  6. Tectonic evolution of the Sevier and Laramide belts within the …

  7. The Confusion Range, west-central Utah: Fold-thrust deformation …

  8. The Role of Shortening in the Sevier Hinterland Within …

    WEBApr 30, 2021 — The Sevier fold-thrust belt is characterized by closely spaced, high-offset, east-vergent thrust-faults and associated folds that generally propagated in-sequence toward the east, and has been …

  9. Knowledge of Utah Thrust System Pushes Forward

    WEBAs the compressional forces declined, the Cordilleran thrust system (including the Sevier thrust belt) was left unsupported. Many of the original thrust faults “relaxed” and slid backwards (to the west).

  10. Sevier orogeny | Mountain Building, Plate Tectonics & Continental ...

  11. Mechanical Properties of the Sevier Desert …

    WEBApr 19, 2018 — The Gunnison thrust (GT) is both the youngest and structurally lowest fault, which uses the same basal décollement inclined at β D as other thrusts (Figure 2a). The Canyon Range thrust (CRT) is in …

  12. Stratigraphy and structure of the Sevier thrust belt and proximal ...

  13. Faulty foundations: Early breakup of the southern Utah …

  14. 34.1: Western Mesozoic Orogenies - Geosciences LibreTexts

  15. Western Mesozoic Orogenies – Historical Geology

  16. Regional structure and kinematic history of the Sevier fold-and …

  17. The Kanarra fold-thrust structure—the leading edge of the Sevier …

  18. Digital Geology of Idaho - Thrust Belt - Idaho State University

  19. (A) Generalized geologic map of the Sevier orogenic belt, …

  20. Stratigraphy and structure of the Sevier thrust belt and proximal ...

  21. Structural evolution of the Sevier fault - Keck Geology Consortium

  22. New age controls on initiation and timing of foreland belt thrusting …

  23. FF-1709-utah - geosociety.org

  24. Craton deformation from flat-slab subduction and rollback

  25. This fault could pose a bigger threat than the San Andreas. Is LA …

  26. From New York to Riyadh, Sabalenka’s season keeps breaking …

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