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Upland California

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Journal Article
Published: 01 February 1999
Bulletin of the Seismological Society of America (1999) 89 (1): 317–324.
... on a Seafloor Recording of the 1990 Upland, California, Earthquake: Implications for Ground Motions from a Larger Earthquake by Dav id M. Boore Abstract The velocity and displacement time series from a recording on the sea- floor at 74 km from the 1990 Upland earthquake (M = 5.6) are dominated by late- arriving...
Journal Article
Published: 01 June 1990
Bulletin of the Seismological Society of America (1990) 80 (3): 507–518.
...Jim Mori; Stephen Hartzell Abstract We examined short-period P waves to investigate if waveform data could be used to determine which of two nodal planes was the actual fault plane for a small ( M L 4.6) earthquake near Upland, California. We removed path and site complications by choosing a small...
Image
Envelope delays for the recording of the 1990 Upland, California, earthquake at station S3E, with log axis for the abscissa. The straight lines were fit by eye and were used to represent the mean envelope delay for use in the stochastic modeling. The envelope delays were not smoothed.
Published: 01 June 2003
Figure 9. Envelope delays for the recording of the 1990 Upland, California, earthquake at station S3E, with log axis for the abscissa. The straight lines were fit by eye and were used to represent the mean envelope delay for use in the stochastic modeling. The envelope delays were not smoothed.
Journal Article
Published: 01 November 1992
Earthquake Spectra (1992) 8 (4): 605–633.
...Bruce F. Maison, M.EERI; Carlos E. Ventura, M.EERI The authors investigate the seismic behavior of an existing base isolated building and interpret its recorded response to the 1990 Upland California earthquake. They formulate a linear-elastic model that accurately represents the building during...
Journal Article
Published: 01 October 1990
Bulletin of the Seismological Society of America (1990) 80 (5): 1162–1179.
...Douglas S. Dreger; Donald V. Helmberger Abstract Three-component broadband waveforms of two small earthquakes near Upland, California, recorded on the Pasadena broadband, high dynamic range instrument, were modeled to obtain useful Green's functions for this path and to examine the sensitivity...
Journal Article
Published: 01 November 1936
American Mineralogist (1936) 21 (11): 715–718.
...Richard Merriam; J. D. Laudermilk Abstract Exceptionally pure diopsides occur in the limestone contact zones at Crestmore near Riverside, and at Cascade Canyon near Upland, California. Chemical analyses and optical properties of both samples, especially that from Cascade Canyon, are close...
Image
Simulation using frequency-dependent correction to phase given by envelope delay of the 1990 Upland, California, earthquake recorded at station S3E, as well as the relative site response as discussed in the text. Shown are the acceleration, velocity, and displacement of the simulations (with and without basin amplification and envelope delay) and the observed motions at S3E from the 1990 Upland earthquake (74 km epicentral distance and M 5.6).
Published: 01 June 2003
Figure 11. Simulation using frequency-dependent correction to phase given by envelope delay of the 1990 Upland, California, earthquake recorded at station S3E, as well as the relative site response as discussed in the text. Shown are the acceleration, velocity, and displacement of the simulations
Image
Frequency versus envelope delay for acceleration, velocity, and displacement time series for the S3E recording of the 1990 Upland, California, earthquake. As expected, the envelope delays are almost identical. The envelope delays were not smoothed.
Published: 01 June 2003
Figure 4. Frequency versus envelope delay for acceleration, velocity, and displacement time series for the S3E recording of the 1990 Upland, California, earthquake. As expected, the envelope delays are almost identical. The envelope delays were not smoothed.
Image
Instantaneous frequency (gray lines) for the Santa Cruz recording of the 1989 Loma Prieta, California, earthquake and the S3E recording of the 1990 Upland, California, earthquake. The ordinate labels for the instantaneous frequency are given on the right axes. The top two panels are for acceleration, and the same scaling has been used for instantaneous frequency in both panels. Note that the scaling for the instantaneous frequency differs for the acceleration, velocity, and displacement time series in the bottom three panels. The instantaneous frequency was smoothed with a triangular smoothing operator having a base width of 5 sec.
Published: 01 June 2003
Figure 2. Instantaneous frequency (gray lines) for the Santa Cruz recording of the 1989 Loma Prieta, California, earthquake and the S3E recording of the 1990 Upland, California, earthquake. The ordinate labels for the instantaneous frequency are given on the right axes. The top two panels
Image
Acceleration, velocity, and displacement horizontal-component time series and envelopes (for the displacement) for the ocean-bottom (station S3E) recording of the 1990 Upland, California, M 5.6 earthquake (orientation of horizontal component unknown, low-cut filtered at 0.1 Hz; see Boore and Smith [1999], Boore [1999]; data available from http://quake.usgs.gov/~boore) and for the University of California Santa Cruz (Lick Laboratory) recording of the 1989 Loma Prieta, California, M 6.9 earthquake (east–west component, low-cut filtered with a ramp from 0.05 to 0.1 Hz; data from the California Strong Motion Instrumentation Program, ftp://ftp.consrv.ca.gov/pub/dmg/csmip/LomaPrieta89/). rep and rjb are epicentral and Joyner–Boore distances, respectively (see Abrahamson and Shedlock, 1997). Note the different timescales for the two recordings.
Published: 01 June 2003
Figure 1. Acceleration, velocity, and displacement horizontal-component time series and envelopes (for the displacement) for the ocean-bottom (station S3E) recording of the 1990 Upland, California, M 5.6 earthquake (orientation of horizontal component unknown, low-cut filtered at 0.1 Hz; see
Image
Observed and predicted 5% damped pseudo relative velocity response spectra (PSV) for the horizontal components of motion at station S3E from the 1990 Upland, California, earthquake. The solid lines are from the data: the thick and thin lines are the PSV from the whole record and from the S-wave portion of the record (the first 50 sec of record shown in Fig. 1), respectively. The spectra are the geometric mean of the spectra for the two horizontal components. The dashed lines are from empirical regression equations published by Abrahamson and Silva (1997) and Boore et al. (1997), and the dots are theoretical predictions assuming body-wave arrivals and the source model of Atkinson and Boore (1998) (AB98). (Modified from Boore [1999].)
Published: 01 June 2003
Figure 8. Observed and predicted 5% damped pseudo relative velocity response spectra (PSV) for the horizontal components of motion at station S3E from the 1990 Upland, California, earthquake. The solid lines are from the data: the thick and thin lines are the PSV from the whole record and from
Series: GSA Special Papers
Published: 15 February 2024
DOI: 10.1130/2024.2562(01)
EISBN: 9780813795621
... on differences in burn patterns in riparian versus upland zones and their implications for stream characteristics. We studied fire patterns and postfire vegetation trajectories in riparian versus upland areas across 26 stream sites in coastal southern California over 12 years, as well as the relationships...
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Series: Miscellaneous Publication
Published: 01 January 1998
DOI: 10.32375/1998-MP46.7
EISBN: 9781732014879
... (tidelands) and recent trends to develop this potential while providing increased environmental protection using “extended reach drilling” from existing onshore (upland) sites. Investigation of the economic feasibility as well as the regulatory and permitting process in developing California’s offshore...
Journal Article
Published: 01 April 1993
Bulletin of the Seismological Society of America (1993) 83 (2): 330–346.
...) . Source inversion of the 1988 Upland, California, earthquake: determination of a fault plane for a small event , Bull. Seism. Soc. Am. 80 , 507 - 518 . Orowan E. (1960) . Mechanism of seismic faulting , Geol. Soc. Am. Mem. 79...
Journal Article
Journal: Geosphere
Published: 29 December 2023
Geosphere (2024) 20 (1): 214–236.
...Antonio F. García; Shannon A. Mahan Abstract Stream-terrace morphostratigraphy and optically stimulated luminescence (OSL) geochronology indicate that storm-driven sedimentation has caused down-system decoupling of the uppermost reaches of McMillan Creek (southern California, USA) from the lower...
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Journal Article
Journal: Geology
Published: 01 December 2013
Geology (2013) 41 (12): 1215–1218.
... both the incising, adjusting lowland and the unadjusted, relict upland, the integrated 10 Be concentrations still provide a denudation rate averaged across the two domains. Because field samples can provide only a snapshot of the current upstream-averaged erosion rate, we employ a numerical landscape...
FIGURES
Journal Article
Published: 01 November 2012
Journal of Paleontology (2012) 86 (6): 973–978.
... smaller than Uintasorex montezumicus from California. Both the newly described taxon and U. montezumicus are among the smallest plesiadapiforms yet known with body weights estimated to be 20 to 25 g. The sediments of the Cathedral Bluffs Tongue of the Wasatch Formation at South Pass contain a unique...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 1978
GSA Bulletin (1978) 89 (3): 321–333.
...LAUREN WRIGHT; EUGENE G. WILLIAMS; PRESTON CLOUD Abstract A late pre-Phanerozoic platform, almost continuously blanketed by algal mats, is recorded in the distributional pattern, composition, and textures of the Noonday Dolomite, Death Valley region, California. The platform, apparently L-shaped...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1959
AAPG Bulletin (1959) 43 (1): 253–254.
...J. R. Evans ABSTRACT The Mescal Range, approximately 33 miles east of Baker, is in the central Mojave desert region of southeastern California. Here exposed, are rocks ranging in age from Precambrian to Recent. There are, however, no known sedimentary rocks of Tertiary age. Paleozoic sedimentary...
Journal Article
Published: 01 June 2003
Bulletin of the Seismological Society of America (2003) 93 (3): 1132–1143.
...Figure 9. Envelope delays for the recording of the 1990 Upland, California, earthquake at station S3E, with log axis for the abscissa. The straight lines were fit by eye and were used to represent the mean envelope delay for use in the stochastic modeling. The envelope delays were not smoothed. ...
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