Publications
Filter Total Items: 7615
Manual del McVCO 1999 Manual del McVCO 1999
El McVCO es un generador de frecuencias basado en un microcontrolador que reemplaza al oscilador controlado por voltaje (VCO) utilizado en telemetría analógica de datos sísmicas. Acepta señales de baja potencia desde un sismómetro y produce una señal subportadora modulada en frecuencia adecuada para enlaces telefónicos o vía radio a un lugar remoto de recolección de datos. La frecuencia...
Authors
P.J. McChesney
A physically-based earthquake recurrence model for estimation of long-term earthquake probabilities A physically-based earthquake recurrence model for estimation of long-term earthquake probabilities
A physically-motivated model for earthquake recurrence based on the Brownian relaxation oscillator is introduced. The renewal process defining this point process model can be described by the steady rise of a state variable from the ground state to failure threshold as modulated by Brownian motion. Failure times in this model follow the Brownian passage time (BPT) distribution, which is...
Authors
William L. Ellsworth, Mark V. Matthews, Robert M. Nadeau, Stuart P. Nishenko, Paul A. Reasenberg, Robert W. Simpson
Rock-fall potential in the Yosemite Valley, California Rock-fall potential in the Yosemite Valley, California
We used two methods of estimating rock-fall potential in the Yosemite Valley, California based on (1) physical evidence of previous rock-fall travel, in which the potential extends to the base of the talus, and (2) theoretical potential energy considerations, in which the potential can extend beyond the base of the talus, herein referred to as the rock-fall shadow. Rock falls in the...
Authors
Gerald F. Wieczorek, Meghan M. Morrissey, Giulio Iovine, Jonathan W. Godt
Calibration formulae and values for velocity seismometers used in the 1998 Santa Clara Valley, California seismic experiment Calibration formulae and values for velocity seismometers used in the 1998 Santa Clara Valley, California seismic experiment
Eaton (1975), Bakun and Dratler (1976), Eaton (1977), Healy and O’Neil (1977), Asten (1977), Stewart and O'Neill (1980), Liu and Peselnick (1986), Eaton (1991), Rodgers et al. (1995), and many others (see Asten (1977) for a list of earlier references) have presented formulae for calculating the damped generator constant (or motor constant), and the damping constant (or fractional damping...
Authors
Allan Goddard Lindh, Jerry P. Eaton, Mary O’Neill Allen, John H. Healy, Samuel W. Stewart, Lu Damerell
Earthquake probabilities in the San Francisco Bay region: 2000 to 2030 - A summary of findings Earthquake probabilities in the San Francisco Bay region: 2000 to 2030 - A summary of findings
The San Francisco Bay region sits astride a dangerous “earthquake machine,” the tectonic boundary between the Pacific and North American Plates. The region has experienced major and destructive earthquakes in 1838, 1868, 1906, and 1989, and future large earthquakes are a certainty. The ability to prepare for large earthquakes is critical to saving lives and reducing damage to property...
Authors
Development of a technically consistent, qualified lithostratigraphic data base for the Yucca Mountain Project Development of a technically consistent, qualified lithostratigraphic data base for the Yucca Mountain Project
Studies of Yucca Mountain, Nevada, as a potential geologic nuclear-waste repository began in the late 1970s and continued to 1988 when the U. S. Nuclear Regulatory Commission determined that the quality assurance (QA) programs in place were not adequate and demanded restructuring to a new QA program. The new QA program was accepted in 1989, but many activities did not resume until new...
Authors
David C. Buesch, R.W. Spengler, M.S. Witkowski, S.M. Keller
Deformation following the 1994 Northridge Earthquake (M=6.7), Southern California Deformation following the 1994 Northridge Earthquake (M=6.7), Southern California
Following the 1994 Mw=6.7 Northridge earthquake, a 65‐km‐long, north‐south array of 11 geodetic monuments was established across the rupture. The array was surveyed with GPS ten times in the 4.25 yr after the earthquake. Although there is evidence for modest nonlinear postseismic relaxation in the first few weeks after the Northridge earthquake, the deformation in the subsequent four...
Authors
James C. Savage, Jerry L. Svarc, W.H. Prescott, Kenneth W. Hudnut
Deformation across the rupture zone of the 1964 Alaska earthquake, 1993–1997 Deformation across the rupture zone of the 1964 Alaska earthquake, 1993–1997
A linear array of 15 geodetic monuments was installed in 1993 across the rupture zone of the 1964 Alaska earthquake (Mw = 9.2). The array extends from Middleton Island (at the edge of the continental shelf and 80 km from the Alaska‐Aleutian trench) to north of Palmer, Alaska (380 km from the trench), in the approximate direction of Pacific‐North American plate convergence (N15.5°W). The...
Authors
James C. Savage, Jerry L. Svarc, W.H. Prescott, W.K. Gross
Weakness of the lower continental crust: A condition for delamination, uplift, and escape Weakness of the lower continental crust: A condition for delamination, uplift, and escape
We discuss three interconnected processes that occur during continental compression and extension: delamination of the lower crust and sub-crustal lithosphere, escape tectonics (i.e., lateral crustal flow), and crustal uplift. We combine calculations of lithospheric viscosity–depth curves with geologic observations and seismic images of the deep crust to infer the mechanisms controlling...
Authors
R. Meissner, Walter D. Mooney
Rumbling geysers (and volcanoes) Rumbling geysers (and volcanoes)
No abstract avaialable.
Authors
Bruce R. Julian
El Nino 1997-98; damaging landslides in the San Francisco Bay area El Nino 1997-98; damaging landslides in the San Francisco Bay area
No abstract available.
Authors
Lynn M. Highland, J. W. Godt, D. G. Howell, W. Z. Savage
Migration of fluids beneath Yellowstone caldera inferred from satellite radar interferometry Migration of fluids beneath Yellowstone caldera inferred from satellite radar interferometry
Satellite interferometric synthetic aperture radar is uniquely suited to monitoring year-to-year deformation of the entire Yellowstone caldera (about 3000 square kilometers). Sequential interferograms indicate that subsidence within the caldera migrated from one resurgent dome to the other between August 1992 and August 1995. Between August 1995 and September 1996, the caldera region...
Authors
Charles W. Wicks, Wayne R. Thatcher, Daniel Dzurisin