Publications
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Traveltimes and amplitudes from nuclear explosions; Nevada Test Site to Ordway, Colorado
This paper treats the results of a study of seismic waves generated by eight nuclear explosions and recorded at 31 locations between the Nevada Test Site (NTS) and Ordway, Colorado. The line of recording stations crosses the eastern part of the Basin and Range Province, the Colorado Plateau, the southern Rocky Mountains, and extends into the Great Plains. In the eastern Basin and Range Province an
Authors
Alan Ryall, David J. Stuart
Crustal structure in the western United States; study of seismic propagation paths and regional traveltimes in the California-Nevada region
The U.S. Geological Survey, with the assistance of United ElectroDynamics, Inc., completed ten weeks of seismic-refraction field work during the summer of 1962 in the southwestern part of the United States. This work was a continuation of a program initiated in 1961 to study traveltimes and seismic propagation paths in the earth?s crust and upper mantle in the western United States. A total of 761
Authors
J.C. Roller, W. H. Jackson, J.F. Cooper, B.A. Martina
Structure of the crust and upper mantle in the western United States
Seismic waves generated by underground nuclear and chemical explosions have been recorded in a network of nearly 2,000 stations in the western conterminous United States as a part of the VELA UNIFORM program. The network extends from eastern Colorado to the California coastline and from central Idaho to the border of the United States and Mexico. The speed of compressional waves in the upper-mantl
Authors
L. C. Pakiser
Preliminary report on seismic-reflection studies of crustal structure in the western, central, and southern United States
During 1963 the U.S. Geological Survey, with the assistance of United ElectroDynamics, Inc., recorded five separate reversed seismic profiles. In addition to these profiles, the U.S. Geological Survey participated in a seismic-calibration program for the DRIBBLE experiment at Tatum Dome, Mississippi, a 20,000-pound shot near Dexter, Missouri, and in a cooperative seismic experiment in the Lake Sup
Authors
J.C. Roller, O.P. Strozier, W. H. Jackson, J. H. Healy
A progress report on seismic model studies
The value of seismic-model studies as an aid to understanding wave propagation in the Earth's crust was recognized by early investigators (Tatel and Tuve, 1955). Preliminary model results were very promising, but progress in model seismology has been restricted by two problems: (1) difficulties in the development of models with continuously variable velocity-depth functions, and (2) difficulties i
Authors
J. H. Healy, G. B. Mangan
Preliminary report on landslides in a part of the Orinda Formation, Contra Costa County, California
No abstract available.
Authors
Dorothy Hill Radbruch, Louise M. Weiler
Geomagnetic polarity epochs and pleistocene geochronometry
[No abstract available]
Authors
A. Cox, Richard R. Doell, G. B. Dalrymple
Geomagnetic polarity epochs: Sierra Nevada II
Ten new determinations on volcanic extrusions in the Sierra Nevada with potassium-argon ages of 3.1 million years or less indicate that the remanent magnetizations fall into two groups, a normal group in which the remanent magnetization is directed downward and to the north, and a reversed group magnetized up and to the south. Thermomagnetic experiments and mineralogic studies fail to provide an e
Authors
A. Cox, Richard R. Doell, G. Brent Dalrymple
Crustal structure in Nevada and southern Idaho from nuclear explosions
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 = 6.15 + Δ/7.84, where time is in seconds and the shot-detector distance (Δ) is in km. Assuming constant velocities and horizontal layers, crusta
Authors
L. C. Pakiser, D. P. Hill
Digital processing of array seismic recordings
This technical letter contains a brief review of the operations which are involved in digital processing of array seismic recordings by the methods of velocity filtering, summation, cross-multiplication and integration, and by combinations of these operations (the "UK Method" and multiple correlation). Examples are presented of analyses by the several techniques on array recordings which were obta
Authors
Alan Ryall, John Birtill
Times and locations of explosions; U.S. Geological Survey 1962 field season
The U.S. Geological Survey detonated 86 large charges of chemical explosives in the western United States from 6 June to 9 August 1962, in a study of crustal structure in the western United States. This Technical Letter consists of two tables containing information about these explosions. Table I gives a brief geographical description of the shotpoints, and Table II gives the date, time, location,
Authors
John C. Roller
Crustal structure along the coast of California from seismic-refraction measurements
Two reversed seismic-refraction profiles were recorded between Los Angeles and San Francisco in 1961. The three shotpoints were located in Santa Monica Bay, offshore near San Francisco, and at Camp Roberts, about halfway between Los Angeles and San Francisco. The velocity of Pg along these profiles is 6.1 ± 0.1 km/sec, with possible exceptions near San Francisco and near Los Angeles, where the sca
Authors
J. H. Healy