14 Geologic Maps, Geophysical Maps, 3-D Geological Models, Digital Mapping Techniques, Map Derivatives, and Digital Map Preparation (Posters)
Monday, 15 April 2024
8:00 AM - 12:00 PM
Grand Ballroom
PRELIMINARY PRECAMBRIAN GEOLOGIC MAP OF THE CENTRAL UNITED STATES
Paper number: 14-3
Program: Theme Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Joseph ColganGeosciences and Environmental Change Science Center, Denver, CO
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Sam JohnstoneGeosciences and Environmental Change Science Center, Denver, CO
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Bryant PlattGeosciences and Environmental Change Science Center, Denver, CO
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Nolan BarretteGeosciences and Environmental Change Science Center, Denver, CO
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Warren P. RoeGeosciences and Environmental Change Science Center, Denver, CO
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Donald SweetkindGeosciences and Environmental Change Science Center, Denver, CO
Abstract
Here we present a preliminary synthesized Precambrian geologic map of the central United States, merged from 11 sources in the National Cooperative Geologic Mapping Program’s (NCGMP) Geologic Map Schema (GeMS) format at a target scale of 1:1,000,000. Faults and contacts are consistently symbolized according to the Federal Geographic Data Committee (FGDC), and about 500 unique units were joined by age and lithology into approximately two dozen compilation units, reflecting a strategy employed in earlier national- and continental-scale geologic maps. Source maps include outcrop information in the Rocky Mountains and Great Lakes where present, but primarily represent compilations of borehole and geophysical data. Prominent structures include the Midcontinent Rift, Medicine Hat block, Wyoming and Superior cratons, Great Falls tectonic zone, and Trans-Hudson and Central Plains orogens. Gaps in western Nebraska highlight the need for new subsurface mapping in the midcontinent. This work supports mineral exploration and resource assessments, as well as scientific research related to paleotectonic models and basin analysis.
Geological Society of America Abstracts with Programs. Vol. 56, No. 2
doi: 10.1130/abs/2024SE-398495
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