Publications
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Hilbert-Huang transform analysis of dynamic and earthquake motion recordings Hilbert-Huang transform analysis of dynamic and earthquake motion recordings
This study examines the rationale of Hilbert-Huang transform (HHT) for analyzing dynamic and earthquake motion recordings in studies of seismology and engineering. In particular, this paper first provides the fundamentals of the HHT method, which consist of the empirical mode decomposition (EMD) and the Hilbert spectral analysis. It then uses the HHT to analyze recordings of hypothetical...
Authors
R.R. Zhang, S. Ma, E. Safak, S. Hartzell
Documentation for 2003 USGS Seismic Hazard Maps for Puerto Rico and the U.S. Virgin Islands Documentation for 2003 USGS Seismic Hazard Maps for Puerto Rico and the U.S. Virgin Islands
No abstract available.
Authors
C.S. Mueller, A.D. Frankel, M.D. Petersen, E. V. Leyendecker
Slip history and dynamic implications of the 1999 Chi-Chi, Taiwan, earthquake Slip history and dynamic implications of the 1999 Chi-Chi, Taiwan, earthquake
[1] We investigate the rupture process of the 1999 Chi‐Chi, Taiwan, earthquake using extensive near‐source observations, including three‐component velocity waveforms at 36 strong motion stations and 119 GPS measurements. A three‐plane fault geometry derived from our previous inversion using only static data [Ji et al., 2001] is applied. The slip amplitude, rake angle, rupture initiation...
Authors
Ji Chen, Donald V. Helmberger, David J. Wald, Kuo-Fong Ma
Lithospheric buoyancy and continental intraplate stresses Lithospheric buoyancy and continental intraplate stresses
Lithospheric buoyancy, the product of lithospheric density and thickness, is an important physical property that influences both the long-term stability of continents and their state of stress. We have determined lithospheric buoyancy by applying the simple isostatic model of Lachenbruch and Morgan (1990). We determine the crustal portion of lithospheric buoyancy using the USGS global...
Authors
M.L. Zoback, Walter D. Mooney
Site response, shallow shear-wave velocity, and wave propagation at the San Jose, California, dense seismic array Site response, shallow shear-wave velocity, and wave propagation at the San Jose, California, dense seismic array
Ground-motion records from a 52-element dense seismic array near San Jose, California, are analyzed to obtain site response, shallow shear-wave velocity, and plane-wave propagation characteristics. The array, located on the eastern side of the Santa Clara Valley south of the San Francisco Bay, is sited over the Evergreen basin, a 7-km-deep depression with Miocene and younger deposits...
Authors
S. Hartzell, D. Carver, R. A. Williams, S. Harmsen, A. Zerva
Earthquake recordings from the 2002 Seattle Seismic Hazard Investigation of Puget Sound (SHIPS), Washington state Earthquake recordings from the 2002 Seattle Seismic Hazard Investigation of Puget Sound (SHIPS), Washington state
This report describes seismic data obtained during the fourth Seismic Hazard Investigation of Puget Sound (SHIPS) experiment, termed Seattle SHIPS . The experiment was designed to study the influence of the Seattle sedimentary basin on ground shaking during earthquakes. To accomplish this, we deployed seismometers over the basin to record local earthquakes, quarry blasts, and teleseisms...
Authors
Thomas L. Pratt, Karen L. Meagher, Thomas M. Brocher, Thomas Yelin, Robert Norris, Lynn Hultgrien, Elizabeth Barnett, Craig S. Weaver
The crustal structure from the Altai Mountains to the Altyn Tagh fault, northwest China The crustal structure from the Altai Mountains to the Altyn Tagh fault, northwest China
[1] We present a new crustal section across northwest China based on a seismic refraction profile and geologic mapping. The 1100‐km‐long section crosses the southern margin of the Chinese Altai Mountains, Junggar Accretional Belt and eastern Junggar basin, easternmost Tianshan Mountains, and easternmost Tarim basin. The crustal velocity structure and Poisson's ratio (σ), which provide a...
Authors
Y. Wang, Walter D. Mooney, X. Yuan, R. G. Coleman
Cold cratonic roots and thermal blankets: How continents affect mantle convection Cold cratonic roots and thermal blankets: How continents affect mantle convection
Two-dimensional convection models with moving continents show that continents profoundly affect the pattern of mantle convection. If the continents are wider than the wavelength of the convection cells (-3000 km, the thickness of the mantle), they cause neighboring deep mantle thermal upwellings to coalesce into a single focused upwelling. This focused upwelling zone will have a...
Authors
V.P. Trubitsyn, Walter D. Mooney, D.H. Abbott
Three-dimensional velocity structure of crust and upper mantle in southwestern China and its tectonic implications Three-dimensional velocity structure of crust and upper mantle in southwestern China and its tectonic implications
Using P and S arrival times from 4625 local and regional earthquakes recorded at 174 seismic stations and associated geophysical investigations, this paper presents a three‐dimensional crustal and upper mantle velocity structure of southwestern China (21°–34°N, 97°–105°E). Southwestern China lies in the transition zone between the uplifted Tibetan plateau to the west and the Yangtze...
Authors
Chun-Yong Wang, W.W. Chan, Walter D. Mooney
Observing earthquakes triggered in the near field by dynamic deformations Observing earthquakes triggered in the near field by dynamic deformations
We examine the hypothesis that dynamic deformations associated with seismic waves trigger earthquakes in many tectonic environments. Our analysis focuses on seismicity at close range (within the aftershock zone), complementing published studies of long-range triggering. Our results suggest that dynamic triggering is not confined to remote distances or to geothermal and volcanic regions...
Authors
Joan S. Gomberg, P. Bodin, P.A. Reasenberg
Density of the continental roots: Compositional and thermal contributions Density of the continental roots: Compositional and thermal contributions
The origin and evolution of cratonic roots has been debated for many years. Precambrian cratons are underlain by cold lithospheric roots that are chemically depleted. Thermal and petrologic data indicate that Archean roots are colder and more chemically depleted than Proterozoic roots. This observation has led to the hypothesis that the degree of depletion in a lithospheric root depends...
Authors
M.K. Kaban, P. Schwintzer, I.M. Artemieva, Walter D. Mooney
Comments on potential geologic and seismic hazards affecting Mare Island, Solano County, California Comments on potential geologic and seismic hazards affecting Mare Island, Solano County, California
This report was prepared in response to a written request from the City of Vallejo, California, to the U.S. Geological Survey (USGS). By letter of October 4, 2002, the City requested that the USGS "provide advice to the City’s LNG Health and Safety Committee on its review of a potential liquid natural gas project" on the southern portion of Mare Island. The City specifically requested...
Authors
T.L. Holzer, C. M. Wentworth, W. H. Bakun, J. Boatwright, T.E. Brocher, M. Çelebi, W.L. Ellsworth, J.P.B. Fletcher, E.L. Geist, R. W. Graymer, R. E. Kayen, D. K. Keefer, D. H. Oppenheimer, W.U. Savage, David P. Schwartz, R.W. Simpson