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U.S. Geological Survey Crustal Studies Technical Letter Number 4

In cooperation with the Defense Advanced Research Projects Agency

Crustal Structure in Nevada and Southern Idaho from Nuclear Explosions

By L.C. Pakiser and D.P. Hill

1962

Thumbnail of and link to report PDF (29.7 MB)Abstract

The time of first arrival of seismic waves generated by 4 underground nuclear explosions at the Nevada Test Site (NTS) and recorded along a line extending north into southern Idaho is expressed as T0 = 0. 00 + Δ/3.0 (assumed), T1 = 0 .40 + Δ/6.03, and T2 = 6.l5 + Δ/7.84, where time is in seconds and the shot-detector distance (Δ) is in km. Assuming constant velocities and horizontal layers, crustal thickness in the vicinity of NTS was determined to be 28 km. Delays in the traveltime segment T2, which represents Pn, indicate that the crust may thicken to 32 km in northern Nevada. A third phase, expressed as T3 = 14.48 + Δ/7.84, was also recognized and has arrival times appropriate for SPS. Amplitudes of Pn were determined at 7 places from recordings of seismic waves from one underground nuclear explosion (ANTLER).

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Suggested citation:

Pakiser, L.C., and Hill, D.P., 1962, Crustal structure in Nevada and southern Idaho from nuclear explosions: U.S. Geological Survey Crustal Studies Technical Letter Number 4, 26 p. (Available at https://pubs.usgs.gov/misc/tl/0004/.)



Contents

Abstract

Introduction

Traveltimes and velocities

Traveltimes and crustal structure

Comparison with earlier investigators

Intermediate crustal layer

Amplitudes of P

The phase T3

References

Appendixes A and B


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