T169 Aeolian Systems in Time and Space (Posters)
Tuesday, 17 October 2023
8:00 AM - 5:30 PM
Hall B
DETRITAL ZIRCON PROVENANCE OF SAND DUNES IN THE WYOMING WIND CORRIDOR
Paper number: T169-5
Program: Technical Sessions
Time: 8:00 AM – 5:30 PM
Authors
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Lily JacksonCenter for Economic Geology Research, University of Wyoming, Laramie, WY
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Mollie PopeUniversity of Wyoming, Laramie, WY
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Adam TrzinskiUniversity of Wyoming, Laramie, WY
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Jay ChapmanUniversity of Texas at El Paso, El Paso, TX
Abstract
The detrital zircon age distribution of the Killpecker dune field shows major age peaks at 52 and 2534 Ma. Seminoe dune field has major age peaks at 93, 1385, and 1719 Ma, and Ferris has a large peak at 2612 Ma. The major Phanerozoic grain age population for Killpecker dunes may be indicative of the Absaroka Volcanics (43-53 Ma), while major Precambrian age populations in all three dune fields are consistent with published ages of local basement uplifts such as the Wind River Range and the deeply eroded Granite Mountains.
Detrital zircon U-Pb age distributions of samples from the three dune fields suggests that they are strongly influenced by local sediment sources. This is statistically supported by Kolmogorov–Smirnov tests in which the p-values between each dune field are significantly less than 10-3.
Future studies in these dune fields will provide clues to the erosional and depositional systems occurring in the area at the time of the dunes formation about 10,000 years ago. This project provides additional zircon data to the central Wyoming area, as well as further understanding of zircon-rich aeolian deposits that may have future economic value.
Geological Society of America Abstracts with Programs. Vol. 55, No. 6
doi: 10.1130/abs/2023AM-390326
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