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Basement structure beneath Langford Well Lake basin, Fort Irwin, California, based on inversion of gravity data

Open-File Report 2000-518
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https://doi.org/10.3133/ofr00518

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Abstract

Gravity data were used to study the basement structure of Langford Well Lake basin at the U.S. Army National Training Center, Fort Irwin, California. Figure 1 shows the location of the study area. During 1996 and 1999, 290 new gravity stations were measured. These data were merged with existing data to produce a depth-to-basement map, which, in turn was converted to a structure map of the basement surface below alluvial fill. This information can be used to help interpret water flow and reservoir capacity of the basin. In addition, gravity gradients were used to suggest locations of faults through or below alluvial fill. These gradients may be evidence for repositioning or extending mapped faults. The locations of gravity stations are shown in figure 2 plotted on a colored grid of topographic elevations generated from 30 m DEM's (Digital Elevation Models). As shown by figure 3, gravity data used in this study are sufficiently accurate to permit 1-mGal contour intervals. Much of the older regional data in this study area are of lesser quality although they were included because they sufficiently represent regional gravity.

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Publication type Report
Publication Subtype USGS Numbered Series
Title Basement structure beneath Langford Well Lake basin, Fort Irwin, California, based on inversion of gravity data
Series title Open-File Report
Series number 2000-518
DOI 10.3133/ofr00518
Year Published 2000
Language English
Publisher U.S. Geological Survey
Publisher location Reston, VA
Contributing office(s) Geology, Minerals, Energy, and Geophysics Science Center
Description 13 p.
Country United States
State California
Other Geospatial Fort Irwin, Langford Well Lake Basin
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