Master of Science in Geoscience
First Committee Member
Andrew Hanson, Chair
Second Committee Member
Third Committee Member
Graduate Faculty Representative
Number of Pages
Understanding the evolution of large-scale fault systems remains a challenge to geologists and is of critical importance in understanding the dynamics of larger plate tectonic interactions. I mapped the southwestern Frenchman Mountain Fault (FMF), conducted a basin analysis of units in the footwall of the fault, and measured kinematic indicators along the fault zone in order to constrain fault offset, magnitude, and timing in an attempt to further our understanding of these systems.
My findings include: 1) the presence of vertical and sub-vertical slickenlines on southwest dipping fault surfaces indicative of normal sense offset; 2) relatively little lateral variation in stratigraphy within the adjacent basin indicating basin-fill being shed directly across the fault, supported by paleocurrent data; and 3) no kinematic evidence indicative of strike-slip motion. I conclude that normal sense displacement on the fault ceased prior to deposition of the Red Sandstone. In addition, I hypothesize that the southwestern FMF is not the Frenchman Mountain block-bounding fault; instead it is buried beneath younger sediments farther to the southwest.
Basin analysis; Basins (Geology); Earth sciences; Frenchman Mountain Fault; Fault zones; Geologic mapping; Geological mapping; Grabens (Geology); Nevada – Las Vegas Valley; Stratigraphy; Structural geology
Earth Sciences | Geology | Geophysics and Seismology | Tectonics and Structure
University of Nevada, Las Vegas
Eaton, Laura Margaret, "Determining the Motion and Location of the Frenchman Mountain Fault, Las Vegas, Nevada: A Paired Basin Analysis and Structural Analysis" (2012). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1519.
IN COPYRIGHT. For more information about this rights statement, please visit http://rightsstatements.org/vocab/InC/1.0/