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    Geologic Map of the Rincon Valley Area, Pima County, Arizona, v. 2.0

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    Author
    Richard, S.M.
    Spencer, J.E.
    Youberg, A.
    Ferguson, C.A.
    Issue Date
    2020
    Keywords
    Arizona Geological Survey Digital Geologic Maps
    Cambrian
    Devonian
    Pennsylvanian
    Permian
    Jurassic
    cretaceous
    Proterozoic
    Paleozoic
    Mesozoic
    Tertiary
    Pleistocene
    Holocene
    Rincon Creek
    Vail
    Basin and Range Province
    Pima County
    Rincon Valley
    Diabase
    Pioneer shale
    mylonitic fabric
    cross-section
    marble
    Catalina detachment fault
    granitoids
    Bolsa Quartzite
    Abrigo Formation
    Horquilla Formation
    Earp Formation
    volcanics
    Tuff breccia
    Pantano Formation
    Bisbee Group
    breccia
    silicified rock
    stream deposits
    Holocene alluvium
    colluvium
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    Citation
    Richard, S.M., Spencer, J.E., Youberg, A., and Ferguson, C.A., 2020, Geologic Map of the Rincon Valley Area, Pima County, Arizona: Arizona Geological Survey Digital Geologic Map DGM-44, version 2.0, map scale 1:24,000, 11 p., 1 map sheet and metadata.
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    The bedrock geology of the map area is dominated by several sets of rock units, as follows: (1) Variably mylonitic granitic and gneissic bedrock at the north flank of the map area forms the Rincon Mountains and the footwall of the Catalina detachment fault. The Catalina detachment fault is a Tertiary, moderately to gently southwest dipping normal fault that has tens of kilometers of top-to-the-southwest displacement (>27.5 km displacement estimated by Dickinson, 1991). (2) Complexly deformed Paleozoic carbonate and siliciclastic strata and Proterozoic granitoids and diabase are exposed at the southwestern foot of the Rincon Mountains and above the Catalina detachment fault. (3) The Oligo-Miocene Pantano Formation, which consists of variably tilted conglomerate, sandstone, mudstone, and andesitic lava flows. Farther to the southwest, the Empire Mountains consist of (4) structurally complex Proterozoic and Paleozoic rocks of diverse composition, and (5) a deformed, regionally southeast dipping sequence of siliciclastic sedimentary rocks of the lower Bisbee Group. In some extensive areas, Quaternary stream incision has uncovered unconsolidated to poorly consolidated clastic sedimentary deposits that are typically mantled by colluvium. These deposits are shown on plate 1 as Tertiary and Quaternary deposits, undivided.
    URI
    http://hdl.handle.net/10150/630948
    Additional Links
    https://library.azgs.arizona.edu/item/ADGM-1599607322039-942
    Language
    en
    Series/Report no.
    DGM-44
    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
    32.16
    South Bounding Coordinate
    32.09
    West Bounding Coordinate
    -110.75
    East Bounding Coordinate
    -110.57
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    AZGS Document Repository

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