Aeromagnetic map of Yucca Mountain and surrounding regions, southwest Nevada

Open-File Report 83-616
By:  and 



Magnetic anomalies over Yucca Mountain and surrounding areas are largely caused by variations in magnetic properties and shapes, including structural offsets, of the extensive volcanic units that underlie the region. In a few places the anomalies are caused by intrusions. Correlation between magnetic properties measured from rock samples and those derived from rock unit-magnetic anomaly associations is excellent. Anomaly characteristics, extensive magnetic gradients, and marked changes in the regional magnetic field can be coupled with the magnetic properties of the rock units to delineate structural boundaries. Three major boundaries are indicated by contrasts in regional magnetic expressions. Less extensive but more clearly indicated boundaries in the immediate vicinity of Yucca Mountain are interpreted from a distinctive pairing of northerly-trending linear positive and negative anomalies which are caused by vertical displacement in generally gently dipping volcanic beds. The displacement between beds is located approximately along the border line between the linear anomaly pairs. One series of pairs of more northeasterly trend lies over the general location of a change from moderately thick to very thick volcanic units that was interpreted from gravity data. Several low amplitude but distinctively shaped anomalies in areas underlain primarily by sedimentary strata indicate the presence of intrusions and faults.

Additional publication details

Publication type Report
Publication Subtype USGS Numbered Series
Title Aeromagnetic map of Yucca Mountain and surrounding regions, southwest Nevada
Series title Open-File Report
Series number 83-616
DOI 10.3133/ofr83616
Edition -
Year Published 1983
Language ENGLISH
Publisher U.S. Geological Survey,
Description i, 19 p. :maps ;28 cm.; 1 over-size sheet; scale 1:48000 (1 inch = 4000 feet)
Scale 48000
Google Analytic Metrics Metrics page
Additional metadata about this publication, not found in other parts of the page is in this table