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Notes on some experiments on the application of subtractive compensation to USGS seismic magnetic tape recording and playback systems Notes on some experiments on the application of subtractive compensation to USGS seismic magnetic tape recording and playback systems

The purpose of these experiments is to lay the groundwork for the implementation of subtractive compensation of the USGS seismic network tape playbacks utilizing the Develco model 6203 discriminators at a x1 playback speed. Although the Develco discriminators were designed for this application and a matching Develco compensation discriminator was purchased, effective use of this system...
Authors
Jerry P. Eaton

Earthquake mechanism and displacement fields close to fault zones: Report on the Sixth GEOP Research Conference Earthquake mechanism and displacement fields close to fault zones: Report on the Sixth GEOP Research Conference

The Sixth Geodesy/Solid Earth and Ocean Physics (GEOP) Research Conwas held on February 4–5, 1974, at the Institute of Geophysics and Planetary Physics, University of California, San Diego, in La Jolla, California. It was attended by about 100 persons. James N. Brune, program chairman, opened the conference and delivered the introductory address, a somewhat extended version of which is...
Authors
Craig R. Allen, Jon Berger, Ivan I. Mueller, James C. Savage, J. Weertman

Geodetic determination of strain at the Nevada Test Site following the Handley event Geodetic determination of strain at the Nevada Test Site following the Handley event

Repeated surveys of a trilateration network (aperture greater than 20 km) centered on ground zero for the HANDLEY event, a nuclear explosion at the Nevada Test Site with yield in excess of 1 megaton, suggest that the explosion induced an east-west extension of the network by more than 50 mm. In the year following the detonation, this deformation reversed such that the final configuration
Authors
James C. Savage, W. T. Kinoshita, W.H. Prescott

Effects of the Bear Valley and San Juan Bautista earthquakes of 1972 on Geodimeter line lengths Effects of the Bear Valley and San Juan Bautista earthquakes of 1972 on Geodimeter line lengths

Measurements of lines of the California Geodimeter network in the vicinity of the epicenters of four 1972 earthquakes (magnitudes 4.7, 4.7, 4.8, and 5.1) along the San Andreas fault system indicate that no significant anomalous changes in line length preceded or accompanied those earthquakes. Within the precision of measurement, the data are consistent with a linear change in line length...
Authors
W.H. Prescott, James C. Savage

Selected chlorinated hydrocarbons in bottom material from streams tributary to San Francisco Bay Selected chlorinated hydrocarbons in bottom material from streams tributary to San Francisco Bay

As part of a study of the environmental quality of San Francisco Bay, bottom material from 26 streams tributary to the Bay were analyzed for chlordane, DDD, DDE, DDT, and PCB residues. These compounds were present in essentially all streams tested. Chlordane proved to be ubiquitous, with a concentration range similar to that of the other compounds. Noteworthy was the occurrence in one...
Authors
LeRoy M. Law, Donald F. Goerlitz

Tectonic significance of the Kodiak-Bowie seamount chain, northeastern Pacific Tectonic significance of the Kodiak-Bowie seamount chain, northeastern Pacific

The hypothesis of a fixed melting spot reference frame (M) for relative plate motion is tested in the northeastern Pacific Ocean, where the Kodiak-Bowie seamount chain intersects the northern triple junction between the Pacific, American, and Juan de Fuca plates. Available age determinations on Kodiak and Giacomini Seamounts provide an estimated average rate of volcanic propagation along...
Authors
Eli A. Silver, Roland E. von Huene, James K. Crouch

Effects of local geology on ground motion in the San Francisco Bay region, California: A continued study Effects of local geology on ground motion in the San Francisco Bay region, California: A continued study

Measurements of ground motion generated by nuclear explosions in Nevada have been completed for 99 locations in the San Francisco Bay region, California. The seismograms, Fourier amplitude spectra, spectral amplification curves for the signal, and the Fourier amplitude spectra of the seismic noise are presented for 60 locations. Analog amplifications, based on the maximum signal...
Authors
James F. Gibbs, Roger D. Borcherdt

Geodimeter measurements of slip and strain accumulation along the San Andreas fault Geodimeter measurements of slip and strain accumulation along the San Andreas fault

The U.S. Geological Survey conducts repeated geodimeter surveys of trilateration networks in central California in order to study the processes of slip and strain accumulation along the San Andreas fault. The precision of distance measurement is described by a standard deviation σ = (a2+ b2L2)12 where a = (a2+ b2L2)12 where a = 3mm, b = 2 · 10−7, and L is the line length. Within the...
Authors
J.C. Savage, W.H. Prescott

Structure of the crust in the conterminous United States Structure of the crust in the conterminous United States

On the basis of the newest interpretations of all sufficiently long seismic profiles, a contour map of the Mohorovičić discontinuity for the conterminous United States is compiled. Differences from earlier interpretations are discussed.
Authors
David H. Warren, J. H. Healy

Earthquakes in the oil field at Rangely, Colorado Earthquakes in the oil field at Rangely, Colorado

Seven years of seismic data recorded at the Uinta Basin Observatory were searched for earthquakes originating near an oil field at Rangely, Colorado, located 65 km ESE of the observatory. Changes in the number of earthquakes recorded per year appear to correlate with changes in the quantity of fluid injected per year. Between November 1962 and January 1970, 976 earthquakes were detected...
Authors
James F. Gibbs, John H. Healy, C. Barry Raleigh, John M. Coakley

Man-made earthquakes and earthquake prediction Man-made earthquakes and earthquake prediction

Convincing evidence that man can trigger earthquakes has been developed since the 1963–1967 report. The fact that man can start earthquakes has increased our understanding of earthquake mechanisms and reinforced our judgment that we are approaching the possibility of earthquake prediction. Traditionally, seismologists have avoided the subject of earthquake prediction because of its...
Authors
J. H. Healy, L. C. Pakiser
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