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  2. Thrust faulting in Utah12:
    • Began in northwestern Utah in the latest Jurassic or earliest Cretaceous.
    • Sparse evidence found in Emigration Canyon near Salt Lake City.
    • The Canyon Range, Pavant, Paxton, and Gunnison thrust systems in central Utah form the Sevier fold-and-thrust belt.
    • The Canyon Range thrust carries a thick succession of Neoproterozoic through Triassic sedimentary rocks.
    • The Sevier Desert detachment fault breaches the surface.
    Learn more:
    Thrust faulting began in northwestern Utah in the latest Jurassic or earliest Cretaceous. Sparse evidence is found in Emigration Canyon near Salt Lake City, where boulder conglomerate strata near the base of the Kelvin Formation were derived from the westernmost and oldest thrust sheet.
    geology.utah.gov/map-pub/survey-notes/knowledg…
    The Canyon Range, Pavant, Paxton, and Gunnison thrust systems in central Utah form the Sevier fold-and-thrust belt in its type area. The Canyon Range thrust carries an ∼12-km-thick succession of Neoproterozoic through Triassic sedimentary rocks and is breached at the surface by the Neogene extensional Sevier Desert detachment fault.
    pubs.geoscienceworld.org/gsa/gsabulletin/article-a…
     
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