Monday,
November 11, 2024
6:00 - 7:30 pm
For those attending in-person this meeting
will be held at the following location:
Pellissippi State Community College
Room location is
MC-216
Note: ETGS members participating virtually will receive an email with info for attending/logging into the meeting.
November Presentation
Detrital zircon and rutile U-Pb geochronology of Cretaceous strata in the
eastern Gulf Coastal Plain and its implications for heavy mineral sand
exploration in western Tennessee
By
Authors: William T. Jackson, Jr. (presenter), Joseph Lane, and Barry Shaulis
Geology Supervisor/State Geologist
Tennessee Geological Survey
Abstract
Detrital zircon geochronology
provides valuable information for determining sediment provenance
and characterizing source rock regions. We present detrital zircon
and rutile U-Pb geochronology results from the Cretaceous McNairy
Sand in western Tennessee and the Ripley Formation in Mississippi
and Alabama to reconstruct paleo-drainage systems along the eastern
Gulf Coastal Plain. Results suggest three routing systems with
headwater regions in the southern Appalachian thrust belt. Two
drainages sourced the southern Appalachian, eastern Blue Ridge, and
Inner Piedmont provinces, with one routing sediment to Alabama and
eastern Georgia, while a separate drainage system routed sediment to
western Tennessee. A central drainage system between the
northwestern and southeastern directed drainages sourced material
from the southern Appalachian, western Blue Ridge, and Valley and
Ridge provinces and supplied sediment to northeastern Mississippi.
Alongshore sediment transport from the southeast to the northwest
and local reworking during the Late Cretaceous complicates detrital
geochronology signatures. Late Cretaceous heavy mineral sand
deposits are historically known to be economical viable in
northwestern Tennessee and near the Alabama-Georgia state border. We
suggest that the abundance of heavy minerals is related to sediment
provenance and deposits sourced from the eastern Blue Ridge and
Inner Piedmont exhibit increased proportions of heavy minerals
important for the critical mineral and rare earth element
industries.
Biography
Education
PhD, Geological Sciences, 2017, University of Alabama
MS, Earth Sciences, 2012, University of Memphis
BS, Geology, 2009, University of Alabama
Employment
2024 - Present Geology Supervisor, TDEC, Division of Mineral and
Geologic Resources, Tennessee Geological Survey
2020 - 2024 Assistant Professor, Department of Earth Sciences,
University of Memphis
2017 - 2020 Assistant Professor, Department of Earth Sciences,
University of South Alabama
2015 - 2017 Field Geologist, Geological Survey of Alabama
Interests
I am a field-oriented geoscientist with a focus on tectonic
processes and basin analysis. My research involves the integration
of sedimentology, stratigraphy, and structural geology with
geochronology and thermochronology to understand sediment provenance
and the relationships between deformation and deposition. I have
focused research interests in (a) comparing the Appalachian Mountain
belt to the modern Himalaya-Tibet orogenic system, (b) soft-sediment
deformational structures in the Laramide belt of the Rocky
Mountains, and (c) the eastern Gulf Coastal Plain of Tennessee,
Mississippi, and Alabama.
Research Funding
US Geological Survey (USGS) and National Science Foundation (NSF)
Honors
2018 Stephen E. Laubach Structural Diagenesis Award, Geological
Society of America
Greetings, and welcome to the November 11, 2024 ETGS
hybrid meeting.
If you attend via Zoom as a courtesy please mute your cell phone or the microphone in your laptop/tablet to minimize background noise and feedback echos. We will also make an effort to mute all participants - at least until the presentation is finished. Please use the chat feature to type any comments or questions you may have. We recommend that you send questions for the speaker to "everyone" so all participants can see the question. In the interest of time, we may hold the Q&A at the end of the presentation.
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to be listed on the attendance sheet. Let us know exactly how your
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format. As always, we welcome and appreciate your feedback and
suggestions for improvement.
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