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Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 1977 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 1977

The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.
Authors
J.B. Townshend, J.E. Papp, M.J. Moorman, C.E. Deadmon, S.P. Tilton

Catalog of seismic records obtained in support of the ERDA/Nevada Operations Office, October 1963 through June 1976 Catalog of seismic records obtained in support of the ERDA/Nevada Operations Office, October 1963 through June 1976

The United States Geological Survey (USGS), Branch of Earthquake Hazards (BEH), Las Vegas, Nevada has provided ERDA, Nevada Operations Office, with seismic monitoring support to the underground nuclear weapons test program conducted at the Nevada Test Site (NTS) since September 1961. Activities from September 15, 1961 to September 13, 1963 are summarized in the report, "Seismic Dats...
Authors
R. Navarro, E.D. Sembera, W.L. Jungblut

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: May 1977 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: May 1977

The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.
Authors
J.B. Townshend, J.E. Papp, M.J. Moorman, C.E. Deadmon, S.P. Tilton

Summary of results of frictional sliding studies, at confining pressures up to 6.98 kb, in selected rock materials Summary of results of frictional sliding studies, at confining pressures up to 6.98 kb, in selected rock materials

This report is a collection of stress-strain charts which were produced by deforming selected simuiated fault gouge materials. Several sets of samples consisted of intact cylinders, 1.000 inch in diameter and 2.500 inches long. The majority of the samples consisted of thin layers of the selected sample material, inserted within a diagonal sawcut in a 1.000-inch by 2.500-inch Westerly...
Authors
R. Summers, J. Byerlee

Preseismic and coseismic deformation associated with the Hollister, California, earthquake of November 28, 1974 Preseismic and coseismic deformation associated with the Hollister, California, earthquake of November 28, 1974

The epicenter of the Hollister earthquake (ML = 5.1) of November 28, 1974, is located near the center of an 81‐line trilateration network which has been surveyed annually since 1971. Five lines in the neighborhood of the epicenter were surveyed just 2 days before the earthquake, and two other lines nearby were surveyed 48 days earlier. Although some of these measurements suggest a...
Authors
James C. Savage, Mary Ann Spieth, W.H. Prescott

Strain accumulation on the San Andreas Fault near Palmdale, California Strain accumulation on the San Andreas Fault near Palmdale, California

Precise distance measurements of a 10×25 km 15‐station trilateration network that spans the San Andreas fault west of Palmdale, California, have been repeated annually in the period 1971–1975. The network appears to be deforming under simple uniform tensor shear of about 0.21±0.03 μstrain/yr with the direction of maximum right‐lateral shear parallel to the local strike of the San Andreas...
Authors
W.H. Prescott, James C. Savage

Evidence of post-Pleistocene faults on New Jersey Atlantic outer continental shelf Evidence of post-Pleistocene faults on New Jersey Atlantic outer continental shelf

Recently obtained high-resolution seismic profiles (400-4,000-Hz band) show evidence of faults in shallow sedimentary strata near the edge of the Atlantic continental shelf off New Jersey. Apparent normal faults having a throw of about 1.5 m displace sediments to within 7 m of the sea floor. The faults appear to be overlain by undeformed horizontal beds of relatively recent age. Several...
Authors
R. E. Sheridan, H.J. Knebel

Sclerochronology: a tool for interpreting past environments Sclerochronology: a tool for interpreting past environments

X-radiographs of stony coral slabs reveal two types of annual density bands. Detailed studies of these bands in relation to known variations in air temperatures indicate that sclerochronology is a valid tool for documenting time sequences and changing environmental conditions on a coral reef.
Authors
J. Harold Hudson, Eugene A. Shinn, Robert B. Halley, Barbara H. Lidz
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