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- W245521872 abstract "A Mid-Tertiary horizontal compression, verging radially toward Az 120 to 215 and extending E-W for 90 km across the High Plateaus of SW Utah, was driven by intrusions and/or gravitational spreading of the Marysvale volcanic field, 40-60 km to the north. Structures of this deformation overprint a NNW trending Laramide monocline on the east, and are overprinted by NNE trending Basin and Range extensional structures. To the west at the Sevier deformation front, Mid-Tertiary compressional structures are directed Az 205, but no Sevier foreland deformation was found. Small scale structures of the Laramide, Mid-Tertiary, and Basin and Range deformations are partitioned lithologically in four rock types of different properties: (1) Friable Cretaceous sands contain Laramide and Mid-Tertiary conjugate compressional sand shear wedges or Laramide and Basin and Range conjugate, extensional sand shears; (2) Calcareous Cretaceous sandstones or Eocene Claron Fm limestones contain both conjugate compressional wedge faults and strike-slip faults; (3) spaced dissolution cleavage occurs only in Claron limestones; (4) cretaceous coals contain Mid-Tertiary joints (cleat) at distal locations. A Mid-Tertiary layer-parallel strain gradient toward the SE-S-SSW is marked by deformation fronts in the four rock types where conjugate faults, spaced cleavage, sand shears and joints in coal successively disappear." @default.
- W245521872 created "2016-06-24" @default.
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- W245521872 date "1993-03-01" @default.
- W245521872 modified "2023-09-23" @default.
- W245521872 title "Structural relationships and lithologic deformation partitioning of the Sevier, Laramide, Mid-Tertiary and Basin and Range deformations in the High Plateaus of southwestern Utah" @default.
- W245521872 hasPublicationYear "1993" @default.
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