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    Geologic map of the Picacho Mountains and Picacho Peak, Pinal County, southern Arizona, v. 2.0.

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    DGM 154 Picacho Peak.pdf
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    Author
    Richard, S.M.
    Spencer, J.E.
    Ferguson, C.A.
    Pearthree, P.A.
    Issue Date
    2022
    Keywords
    Picacho Peak
    Picacho Mountains
    Pinal County
    Arizona
    map
    topography
    geomorphology
    Geology
    Proterozoic
    cretaceous
    Quaternary
    Tertiary
    detachment fault
    mylonitic fabric
    Laramide orogeny
    granitoids
    andesites
    Digital Geologic Maps
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    Citation
    Richard, S.M., Spencer, J.E., Ferguson, C.A., and Pearthree, P.A., 2022, Geologic map of the Picacho Mountains and Picacho Peak, Pinal County, southern Arizona, V. 2.0. Arizona Geological Survey Digital Geologic Map, DGM-154, 1 map sheets, map scale 1:24,000, 43 p.
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    The Picacho Mountains are north-south trending mountain range completely surrounded by Quaternary alluvium, and consists of Tertiary and older granitic and gneissic rocks (Figure 1). Picacho Peak, located south of the south end of the range, is also surrounded by alluvium, and consists of Tertiary andesitic volcanic rocks. Picacho Peak and the Picacho Mountains are separated by a gap of shallowly buried bedrock through which pass Interstate 10, the Southern Pacific Railroad, and the Central Arizona Project canal. The Picacho Mountains consists of a compositionally diverse suite of Tertiary, Cretaceous or Proterozoic granitoids, heterogeneous to gneissic granite, muscovite granite, schist, and gneiss, much of which has been affected by middle Tertiary mylonitic deformation and probably by late Cretaceous synplutonic deformation [Rehrig, 1986]. Mylonitization is inferred to have accompanied normal faulting and ascent of the bedrock from mid-crustal depths in the footwall of a moderate to low-angle normal fault commonly known as a "detachment fault". Older gneissic fabrics may record Laramide mid-crustal deformation, or relict Proterozoic fabric. The crystalline rocks of the Picacho Mountains are part of the footwall of a south- to southwest-dipping detachment fault that is exposed in only one small area in the southern Picacho Mountains. Picacho Peak, which consists almost entirely of northeast-dipping basaltic and andesite volcanic rocks, is part of the hanging wall of the detachment fault. Geologic map of the Picacho Mountains and Picacho Peak, Pinal County, southern Arizona - report and two map sheets, scale 1:24,000.
    URI
    http://hdl.handle.net/10150/630820
    Additional Links
    https://library.azgs.arizona.edu/item/ADGM-1663016995674-179
    Language
    en
    Series/Report no.
    DGM - 154
    Rights
    Arizona Geological Survey. All rights reserved.
    Collection Information
    Documents in the AZGS Document Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu.
    North Bounding Coordinate
    32.8727
    South Bounding Coordinate
    32.6024
    West Bounding Coordinate
    -111.443
    East Bounding Coordinate
    -111.294
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    AZGS Document Repository

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