Pliocene-Pleistocene continental deposits in western Kentucky: A new look at regional stratigraphy and depositional history
Abstract
Pliocene and Pleistocene age sediments of the northernmost Mississippi Embayment consist of a thick sequence of continental deposits which rest unconformably on Cretaceous through Eocene strata. The continental deposits have been tentatively correlated to the Pliocene Mounds Gravel and Pleistocene Henry and Equality Formations of southern Illinois. These sediments have previously been interpreted as representing alluvial fan and fluvial deposits. The continental deposits are generally divided into three lithofacies: (1) silt/clay dominated; (2) sand dominated, and (3) gravel dominated. A subsurface study utilizing approximately 300 soil borings has shown that (1) the continental deposits, particularly the gravel facies, exhibit significant local changes in thickness, (2) the upper portion of the sequence consists predominantly of finer-grained silt/clay lithofacies, and (3) sand and gravel lithofacies within the upper sequence often occur at predictable horizons. These observations indicate a paleovalley fill with distinct depositional episodes. As a result of Pleistocene base level fluctuations, stream systems became deeply entrenched in the Pliocene alluvial fan and older sediments. Fan deposits were initially transported and redeposited in a braided fluvial system. As valley alluviation continued and gradients decreased, the braided fluvial system evolved into a meandering system. During Woodfordian time, slackwater lakes created by glacial outwashmore »
- Authors:
-
- Martin Marietta Energy Systems, Inc., Paducah, KY (United States)
- Publication Date:
- OSTI Identifier:
- 6137231
- Report Number(s):
- CONF-921058-
Journal ID: ISSN 0016-7592; CODEN: GAAPBC
- Resource Type:
- Conference
- Journal Name:
- Geological Society of America, Abstracts with Programs; (United States)
- Additional Journal Information:
- Journal Volume: 24:7; Conference: 1992 annual meeting of the Geological Society of America (GSA), Cincinnati, OH (United States), 26-29 Oct 1992; Journal ID: ISSN 0016-7592
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; KENTUCKY; SEDIMENTARY BASINS; STRATIGRAPHY; DEPOSITION; GEOLOGIC HISTORY; LITHOLOGY; PLEISTOCENE EPOCH; PLIOCENE EPOCH; SEDIMENTS; CENOZOIC ERA; DEVELOPED COUNTRIES; GEOLOGIC AGES; GEOLOGIC STRUCTURES; GEOLOGY; NORTH AMERICA; PETROLOGY; QUATERNARY PERIOD; TERTIARY PERIOD; USA; 580000* - Geosciences
Citation Formats
Phillips, B E. Pliocene-Pleistocene continental deposits in western Kentucky: A new look at regional stratigraphy and depositional history. United States: N. p., 1992.
Web.
Phillips, B E. Pliocene-Pleistocene continental deposits in western Kentucky: A new look at regional stratigraphy and depositional history. United States.
Phillips, B E. 1992.
"Pliocene-Pleistocene continental deposits in western Kentucky: A new look at regional stratigraphy and depositional history". United States.
@article{osti_6137231,
title = {Pliocene-Pleistocene continental deposits in western Kentucky: A new look at regional stratigraphy and depositional history},
author = {Phillips, B E},
abstractNote = {Pliocene and Pleistocene age sediments of the northernmost Mississippi Embayment consist of a thick sequence of continental deposits which rest unconformably on Cretaceous through Eocene strata. The continental deposits have been tentatively correlated to the Pliocene Mounds Gravel and Pleistocene Henry and Equality Formations of southern Illinois. These sediments have previously been interpreted as representing alluvial fan and fluvial deposits. The continental deposits are generally divided into three lithofacies: (1) silt/clay dominated; (2) sand dominated, and (3) gravel dominated. A subsurface study utilizing approximately 300 soil borings has shown that (1) the continental deposits, particularly the gravel facies, exhibit significant local changes in thickness, (2) the upper portion of the sequence consists predominantly of finer-grained silt/clay lithofacies, and (3) sand and gravel lithofacies within the upper sequence often occur at predictable horizons. These observations indicate a paleovalley fill with distinct depositional episodes. As a result of Pleistocene base level fluctuations, stream systems became deeply entrenched in the Pliocene alluvial fan and older sediments. Fan deposits were initially transported and redeposited in a braided fluvial system. As valley alluviation continued and gradients decreased, the braided fluvial system evolved into a meandering system. During Woodfordian time, slackwater lakes created by glacial outwash dams produced extensive lacustrine deposits. At least two major episodes of lacustrine sedimentation are apparent. Significant fluctuations of lake level are recognized in the subsurface by local erosional surfaces overlain by coarser-grained sediments deposited in basinward-migrating channel and shoreline facies.},
doi = {},
url = {https://www.osti.gov/biblio/6137231},
journal = {Geological Society of America, Abstracts with Programs; (United States)},
issn = {0016-7592},
number = ,
volume = 24:7,
place = {United States},
year = {Wed Jan 01 00:00:00 EST 1992},
month = {Wed Jan 01 00:00:00 EST 1992}
}