J.C. Roller
J. F. Gibbs
1964
Seismic-refraction measurements from nuclear and chemical explosions were made along a line from the Nevada Test Site (NTS) to Ludlow, California, and additional recordings from nuclear explosions were made southward toward Calexico, California. The time of first arrivals from the Ludlow shotpoint is expressed as T<sub>0</sub> = 0.00 + Δ/2.50 (assumed), T<sub>1</sub> = 1.00 + Δ6.10, T<sub>2</sub> = 2.81 + Δ/6.80, and T<sub>3</sub> = 5.48 + ~7.76, where T is in seconds and distance Δ is in km. First arrival times from NTS fit the lines T<sub>1</sub> = 0.74 + Δ/6.10, T<sub>2</sub> = 2.81 + Δ/6.80 (assumed), T<sub>3</sub> = 6.70 + Δ/8.04 to a distance of 265 km, beyond 265 km T<sub>3</sub> = 5.83 + Δ/7.75. The difference in the apparent velocities of the P<sub>n</sub> (T<sub>3</sub>) arrival is caused by variations in the dip of the Mohorovicic discontinuity. The thickness of the successive layers at NTS are H<sub>0</sub> s 1.0 km (V<sub>0</sub> ~ 2.5 km/sec), H<sub>1</sub> = 13 km (v<sub>1</sub> = 6.1 km/sec), and H<sub>2</sub> = 20 km (v<sub>2</sub> = 6.8 km/ sec); the total crustal thickness is 34 km. The successive crustal layers at Ludlow have a thickness of H<sub>0</sub> = 1.4 km, H<sub>1</sub> = 13 km, and H<sub>2</sub> = 13 km; the total crustal thickness is 27 km.
application/pdf
10.3133/70043887
en
U.S. Geological Survey
Seismic-refraction measurements of crustal structure between Nevada Test Site and Ludlow, California
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