Archived

This content is available here strictly for research, reference, and/or recordkeeping and as such it may not be fully accessible. If you work or study at University of Kentucky and would like to request an accessible version, please use the SensusAccess Document Converter.

Author ORCID Identifier

https://orcid.org/0009-0009-9163-3084

Date Available

8-7-2023

Year of Publication

2023

Document Type

Master's Thesis

Degree Name

Master of Science (MS)

College

Arts and Sciences

Department/School/Program

Geology

Faculty

Dr. Frank Ettensohn

Faculty

Dr. Kevin Yeager

Abstract

The upper Lexington Limestone of Late Ordovician age has been interpreted to represent a structurally controlled, complex, facies mosaic. This facies mosaic has historically been interpreted to be a carbonate buildup of shoal complexes with interbedded shale units with intertonguing facies. Due to relatively recent advances in geographic-information-systems (GIS) mapping technologies, it is possible to generate three-dimensional (3-D) compatible maps to offer insight to the complexities of the upper Lexington Limestone and to determine if structural control affected the distribution of members. The resulting two-dimensional (2-D) and 3-D maps show that basement faults likely exerted a significant influence on facies distribution and formation. The 3-D maps further suggest that post-depositional structural activity during the Alleghanian orogeny resulted in large-scale deformation of the Lexington Limestone to generate structures like the Jessamine Dome.

Digital Object Identifier (DOI)

https://doi.org/10.13023/etd.2023.389

Funding Information

This study was supported by the United States Geological Survey's EDMAP Grant (no.: G22AC00173-00) in 2022-2023.

Share

COinS