Publications
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Earth fissures and localized differential subsidence Earth fissures and localized differential subsidence
Long linear tension cracks associated with declining groundwater levels at four sites in subsiding areas in south-central Arizona, Fremont Valley, California, and Las Vegas Valley, Nevada, occur near points of maximum convex-upward curvature in subsidence profiles oriented perpendicular to the cracks. Profiles are based on repeated precise vertical control surveys of lines of closely...
Authors
Thomas L. Holzer, Earl H. Pampeyan
A comparison of ground response in the Los Angeles region from nuclear explosions and the 1971 San Fernando earthquake A comparison of ground response in the Los Angeles region from nuclear explosions and the 1971 San Fernando earthquake
No abstract available.
Authors
A. M. Rogers, P. A. Covington, Roger D. Borcherdt
Plastic deformation of MgO(A12O2)1·1 spinel at 0·28TM preliminary results Plastic deformation of MgO(A12O2)1·1 spinel at 0·28TM preliminary results
Prism-shaped single crystals of MgO(Al2O3)n spinel (n 1.1) have been compressed to significant plastic strain at a temperature of 400°C (∼0·28 TM) in controlled experiments under a superimposed hydrostatic pressure of 1·4 GPa. Compression of crystals approximately parallel to , and resulted in simple yield behaviour at axial stress differences of 1940, 3720, and 4300 MPa respectively...
Authors
Stephen H. Kirby, P. Veyssiere
Test and calibration of the Seismic Research Observatory Test and calibration of the Seismic Research Observatory
The Seismic Research Observatory (SRO) network is generating an important new data base for seismological research. The SRO systems have extended both the range and resolution of seismic measurements beyond the limits of conventional seismographs and the data are recorded in digital format making it convenient to automate processing and analysis. The SRO network now comprises 12 stations...
Authors
Jon Peterson, Charles R. Hutt, L. Gary Holcomb
Exploratory trench across the Pleasant Valley Fault, Nevada Exploratory trench across the Pleasant Valley Fault, Nevada
An exploratory trench was excavated across the 1915 trace of the Pleasant Valley fault 60 km south of Winnemucca, Nevada, to get information on the history of recent displacements on a fault that had produced a major earthquake in historic time, and on the appearance of such a fault in a trench cut in gravels, sands and silts of an alluvial fan. The trench exposed 16 mappable sedimentary...
Authors
Manuel G. Bonilla, H. A. Villalobos, R. E. Wallace
Nuclear event time histories and computed site transfer functions for locations in the Los Angeles region Nuclear event time histories and computed site transfer functions for locations in the Los Angeles region
This report presents a collection of Nevada Test Site (NTS) nuclear explosion recordings obtained at sites in the greater Los Angeles, Calif., region. The report includes ground velocity time histories, as well as, derived site transfer functions. These data have been collected as part of a study to evaluate the validity of using low-level ground motions to predict the frequency...
Authors
A. M. Rogers, P. A. Covington, R.B. Park, R. D. Borcherdt, D. M. Perkins
In-situ measurements of seismic velocity at 27 locations in the Los Angeles, California region In-situ measurements of seismic velocity at 27 locations in the Los Angeles, California region
Studies conducted in the San Francisco Bay Region (Gibbs, Fumal and Borcherdt, 1980) have shown that average shear-wave velocity can be readily tied to quantitative estimates of ground motion such as ground amplification and earthquake intensity. Furthermore, when certain physical properties of the geologic materials such as texture, hardness and fracture spacing are observed during...
Authors
James F. Gibbs, Thomas E. Fumal, Edward F. Roth
Preliminary observations of noise spectra at the SRO and ASRO stations Preliminary observations of noise spectra at the SRO and ASRO stations
The seismic noise spectra presented in this report were derived from SRO and ASRO station data for the purpose of evaluating the performance of the seismic instruments. They are also useful for constructing a spectral estimate of earth noise at a quiet site based on noise samples obtained from a network of globally distributed sites. It is hoped that the spectra will be usefull for other...
Authors
Jon Peterson
Surface faulting near Livermore, California, associated with the January 1980 earthquakes Surface faulting near Livermore, California, associated with the January 1980 earthquakes
The earthquakes of 24 January (Ms 5.8) 1980 north of Livermore, California, and 26 January (Ms 5.2), were accompanied by surface faulting in the Greenville fault zone and apparently in the Las Positas fault zone also. The surface faulting was discontinuous and of small displacement. The main rupture within the Greenville fault zone trended about N.38°W. It was at least 4.2 km long and...
Authors
Manuel G. Bonilla, James J. Lienkaemper, J. C. Tinsley
U.S. strong-motion programs U.S. strong-motion programs
No abstract available.
Authors
Roger D. Borcherdt, R. B. Matthiesen
Geodolite measurements of deformation near Hollister, California, 1971-1978 Geodolite measurements of deformation near Hollister, California, 1971-1978
A 24‐station trilateration network spanning the San Andreas and Calaveras faults near Hollister, California, has been surveyed each year between 1971 and 1978, inclusive. Two moderate (ML = 5) earthquakes have occurred within the network during the interval. No convincing preseismic or coseismic anomalies associated with those earthquakes have been identified. The deformation of the...
Authors
James C. Savage, W.H. Prescott, Michael Lisowski, N. King
Deformation across the Salton Trough, California, 1973-1977 Deformation across the Salton Trough, California, 1973-1977
A trilateration network extending across the San Andreas, San Jacinto, and Elsinore faults in the vicinity of the Salton Sea, California, has been surveyed to very high precision several times in the 5‐year interval 1973–1977. The average strain across the entire network is essentially a uniaxial north‐south contraction at the rate of about 0.3 μstrain/a. There is no substantial strain
Authors
James C. Savage, W.H. Prescott, Michael Lisowski, N. King