Publications
Filter Total Items: 2585
Proceedings of the 1980 workshop of the International Association of Seismology and Physics of the Earth's Interior on the seismic modeling of laterally varying structures: Contributions based on data from the 1978 Saudi Arabian refraction profile
No abstract available.
Authors
Walter D. Mooney, Claus Prodehl
Noise analysis of the seismic system employed in the northern and southern California seismic nets
The seismic networks have been designed and operated to support recording on Develocorders (less than 40db dynamic range) and analog magnetic tape (about 50 db dynamic range). The principal analysis of the records has been based on Develocorder films; and background earth noise levels have been adjusted to be about 1 to 2 mm p-p on the film readers. Since the traces are separated by only 10 to 12
Authors
J. P. Eaton
Preliminary geologic map of the Colville Indian Reservation, Ferry and Okanogan Counties, Washington, with a table of potassium-argon ages
No abstract available.
Authors
Brian F. Atwater, Robert J. Fleck
Summary geologic report for petroleum lease sale #100, Kodiak Shelf, Alaska
No abstract available.
Authors
M. A. Fisher, Roland E. von Huene, M. A. Hampton
Data from the GEOS digital recorder
No abstract available.
Authors
J. B. Fletcher, Roger D. Borcherdt, C. Mueller, E. Cranswick
A general earthquake observation system (GEOS)
No abstract available.
Authors
Roger D. Borcherdt, Edward G. Jensen, G. Maxwell, J. B. Fletcher, R. McClearn, John R. Van Schaack, R. E. Warrick
Strain‐rate profile across the Elsinore, San Jacinto, and San Andreas Faults near Palm Springs, California, 1973‐81
A profile of the strain accumulation rate along a line trending N50°E across the subparallel Elsinore, San Jacinto, and San Andreas faults near Palm Springs, California, has been constructed from trilateration surveys in the 1973‐81 interval. The strain accumulation is principally right‐lateral shear across a vertical plane parallel to fault strike (N40°W). The strain rate profile for that compone
Authors
N.E. King, James C. Savage
Precision of geodolite surveys: A reply to Jackson and Cheng
Jackson and Cheng have suggested that the changes in areal dilatation measured in Geodolite surveys by the U.S. Geological Survey may be simply an artifact of the measuring system. Although systematic error could conceivably account for the observed excursions in dilatation, we maintain that the specific criticisms by Jackson and Cheng are incorrect: the excursions in dilatation cannot be attribut
Authors
James C. Savage, W. H. Prescott
Strain accumulation in western United States
This review is principally concerned with recent geodetic strain measurements in western United States undertaken by the US Geological Survey as part of the earthquake studies program and, as a consequence, is heavily biased toward the author's own publications. Most of the publications reporting crustal-strain measurements in western United States prior to about 1968 have been compiled in one vol
Authors
James C. Savage
A dislocation model of strain accumulation and release at a subduction zone
Strain accumulation and release at a subduction zone are attributed to stick slip on the main thrust zone and steady aseismic slip on the remainder of the plate interface. This process can be described as a superposition of steady state subduction and a repetitive cycle of slip on the main thrust zone, consisting of steady normal slip at the plate convergence rate plus occasional thrust events tha
Authors
James C. Savage
Deep structure of northern Mississippi embayment
In September 1980, the U. S. Geological Survey conducted a seismic refraction investigation of the northern Mississippi Embayment. During the investigation, 34 shots from nine shotpoints were recorded along a series of profiles. The profiles were parallel to and across an inferred Precambrian rift zone which is outlined by a series of magnetic anomalies and covers an area at least 200 km (125 mi)
Authors
A. Ginzburg, Walter D. Mooney, A.W. Walter, W. J. Lutter, J. H. Healy
Experimental deformation of polycrystalline H2O ice at high pressure and low temperature: Preliminary results
Interest in the mechanical properties of water ice under the conditions in which it exists in the outer solar system has motivated the development and use of a new high‐pressure, low‐temperature triaxial deformation apparatus. Constant displacement rate tests on 70 samples of pure polycrystalline water ice have been performed at temperatures 77≤≤258 K, confining pressures 0.1≤≤350 MPa, and strain
Authors
W. B. Durham, H. C. Heard, Stephen H. Kirby