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    Geologic Map of Volcanic Rocks Along the East Side of Central Chino Valley, Yavapai County, Arizona

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    Author
    Stefanov, W.L.
    Issue Date
    1993
    Keywords
    Arizona Geological Survey Contributed Maps
    Miocene
    Oligocene
    Arizona
    Yavapai County
    Butte 5261
    Sullivan Buttes
    Chino Valley
    Transition Zone
    olivine basalt
    crystallization
    Magma water
    rheology
    volcanic
    amphibole-biotite
    spinel peridotite
    garnet websterite
    clinopyroxenite
    amphibolite
    eclogite
    pyroxene
    Xenocrysts
    Proterozoic
    Paleozoic
    Quaternary
    Tertiary
    Lahar deposits
    Mississippian
    Sullivan buttes latite
    Prescott Granodiorite
    Martin Dolomite
    Redwall Limestone
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    Citation
    Stefanov, W.L., 1993, Geologic Map of Volcanic Rocks Along the East Side of Central Chino Valley, Yavapai County, Arizona: Arizona Geological Survey Contributed Map CM-93-E, map scale 1:12,000, 10 p. and 1 map sheet.
    Publisher
    Arizona Geological Survey (Tucson, AZ)
    Description
    The Sullivan Buttes Latite is an intermediate, high-potassium volcanic rock located in the Transition Zone geologic province of central Arizona. The latite outcrops in Chino Valley, along the southwestern border of the Colorado Plateau. Lava flows, volcaniclastic deposits, and intrusive bodies of latite are found in the Chino Valley area (Tyner 1984). Radiometric dates of 21 to 27 Ma have been obtained from the latite, placing them in the Upper Oligocene to Lower Miocene (Nealey and Sheridan 1989). The latite is of interest as it contains a distinctive xenolith suite. The suite includes eclogite, amphibolite, clinopyroxenite, garnet websterite, granulite, and spinel peridotite (Nealey and Sheridan 1989). Xenocrysts of pyroxene, amphibole, plagioclase and quartz are common in the latite (Tyner 1984), and have been interpreted as originating in the lower crust to upper mantle. The xenoliths have been the subject of considerable study, including work by Arculus and Smith (1979); Schulze and Helmstaedt (1979); and Tyner and Smith (1986). The latite was characterized chemically and petrographically in detail by Tyner (1984), who was able to identify six distinct units within the latite on the basis of geochemistry and mineralogy. These units are amphibole, amphibole-biotite, biotite-pyroxene, mafic, basaltic, and upper latite.
    URI
    http://hdl.handle.net/10150/630622
    Additional Links
    http://repository.azgs.az.gov/uri_gin/azgs/dlio/1095
    Language
    en
    Series/Report no.
    CM-93-E
    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
    34.8
    South Bounding Coordinate
    34.76
    West Bounding Coordinate
    -112.375
    East Bounding Coordinate
    -112.299
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