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slip

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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 June 2017
Lithosphere (2017) 9 (3): 417–430.
... part of the Lenglongling fault. Microtopographic analysis of well-preserved offset terraces, gullies, ridges, and pluvial fans in the highland environment allows evaluation of single-event slip and multievent cumulative slip. Our study provides an important assessment of the horizontal offset...
FIGURES | View All (14)
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 June 2017
Lithosphere (2017) 9 (3): 476–498.
.... Hydrothermal alteration products and mineralization in the core are associated with three highly faulted sections; the lowermost section is associated with the zone of flowing thermal water. Shear slip indicators on faults observed in core indicate slip ranging from pure strike slip to normal failure...
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Journal Article
Published: 01 August 1994
Bulletin of the Seismological Society of America (1994) 84 (4): 1266–1271.
... that is desirable to routinely characterize is the source earthquakes. Combined, these two techniques provide a time function. The source time function contains infor- characterization of the spatio-temporal seismic energy mation about the space-time history of the slip function release between periods of 200...
Journal Article
Published: 01 August 1994
Bulletin of the Seismological Society of America (1994) 84 (4): 1216–1228.
... of earthquakes. It is first assumed that the amplitude of the slip distribution high-pass filtered at high wavenumber does not depend on the size of the ruptured fault. This leads to the following “ k -square” model for the slip spectrum, for k > 1/ L : Δ ~ u L ( k ) = C Δ σ μ L k 2 , where L is the ruptured...
Series: GSA Reviews in Engineering Geology
Published: 01 January 1992
DOI: 10.1130/REG9-p1
EISBN: 9780813758091
... systems (perched water tables) commonly form within compound landslides due to the relatively low permeability of slip-surface gouge, which may slow recharge from the overlying secondary landslides to the host landslide. Movement-inducing pore-fluid pressures can often be reached more rapidly in secondary...
Series: GSA Reviews in Engineering Geology
Published: 01 January 1992
DOI: 10.1130/REG9-p63
EISBN: 9780813758091
Journal Article
Published: 01 October 1991
Bulletin of the Seismological Society of America (1991) 81 (5): 1603–1621.
...Gregory C. Beroza Abstract I have analyzed records from 20 strong-motion instruments that recorded the 1989 Loma Prieta earthquake ( M L = 6.9) to determine the spatial and temporal distribution of slip using a tomographic back-projection technique. I find that the earthquake ruptured bilaterally...
Journal Article
Published: 01 April 1988
Bulletin of the Seismological Society of America (1988) 78 (2): 924–930.
...S. Das Abstract It is shown from numerical experiments that the average slip (and seismic moment) due to the fracture of multiple asperities on a rectangular fault is independent of the distribution of the asperities on the fault for all practical purposes, as long as the average stress drop...
Journal Article
Journal: Geology
Published: 01 August 1985
Geology (1985) 13 (8): 569–572.
...Marie D. Jackson; Paul T. Delaney Abstract We present graphical and analytical methods to determine the extensional or contractional separation of a faulted planar marker using commonly measured field data: fault attitude, slip direction, and bedding or other marker-plane attitude...
Journal Article
Published: 01 June 1985
Bulletin of the Seismological Society of America (1985) 75 (3): 811–833.
...John N. Louie; Clarence R. Allen; David C. Johnson; Paul C. Haase; Stephen N. Cohn Abstract Measurements of slip on major faults in southern California have been performed over the past 18 yr using principally theodolite alignment arrays and tautwire extensometers. They provide geodetic control...
Journal Article
Published: 01 December 1984
Bulletin of the Seismological Society of America (1984) 74 (6): 2593–2611.
.... Of the various sensitivity analyses performed, it is observed that slip rate has the largest effect on exceedence probabilites computed from the stochastic time-predictable model. Therefore, accurate determinations of slip rates (both seismic and aseismic) can substantially reduce the uncertainty in seismic...
Journal Article
Journal: Geology
Published: 01 November 1983
Geology (1983) 11 (11): 674.
Journal Article
Journal: GSA Bulletin
Published: 01 May 1980
GSA Bulletin (1980) 91 (5): 307–312.
... veneers with lubricated interfaces exhibit the same magnitudes of “bedding-plane” slip and somewhat more variability in the senses of slip than do specimens not lubricated. With lubrication, however, there is less deformation of the leading edge of the forcing block, less extensile faulting...
Journal Article
Published: 01 February 1980
Bulletin of the Seismological Society of America (1980) 70 (1): 185–201.
... correlate with the discontinuities in the trace that terminate the segment. The 1970 to 1976 deficit in seismic slip within the segment suggests that fault creep accounts for a significant part of cumulative slip within the segment. The pattern of seismicity is consistent with the hypothesis that creep...
Journal Article
Published: 01 October 1978
Bulletin of the Seismological Society of America (1978) 68 (5): 1421–1448.
...Kebby E. Sieh abstract Historical records indicate that several meters of lateral slip along the San Andreas fault accompanied the great 1857 earthquake in central and southern California. These records, together with dendrochronological evidence, suggest that the rupture occurred along 360 to 400...
Journal Article
Published: 01 August 1978
Bulletin of the Seismological Society of America (1978) 68 (4): 1191–1193.
...P. W. Harsh; N. Pavoni Copyright © 1978, by the Seismological Society of America References Burford R. O. (1972) . Continued slip on the Coyote Creek fault after the Borrego Mountain earthquake , in The Borrego Mountain...
Journal Article
Published: 01 August 1978
Bulletin of the Seismological Society of America (1978) 68 (4): 999–1011.
...Eugene L. Chez; J. Dundurs; Maria Comninou abstract The reflection of elastic waves is customarily treated by assuming that the interface neither separates nor slips. This paper considers the reflection of SH waves that are strong enough to break friction between two solids which are pressed...
Journal Article
Published: 01 August 1978
Bulletin of the Seismological Society of America (1978) 68 (4): 1187–1190.
...R. P. Keller; C. R. Allen; R. Gilman; N. R. Goulty; J. A. Hileman 16 1 1978 Copyright © 1978, by the Seismological Society of America References Burford R. O. (1972) . Continued slip on the Coyote Creek fault...
Journal Article
Published: 01 February 1978
Bulletin of the Seismological Society of America (1978) 68 (1): 155–168.
... parameters to details of the tilt wave forms. The tilt time histories, source-station configuration, and the displacement time history can be used to infer the type and amount of the displacement, the propagation direction and depth of the slip zone. The shallow depth and finite size of the slip zone...
Journal Article
Published: 01 August 1977
Canadian Journal of Earth Sciences (1977) 14 (8): 1953–1958.
...Iain Allison; Timothy E. La Tour Abstract Hornblende in a mylonitic rock from the Grenville front has deformed by fracture and slip on a parting subnormal to the c crystallographic axis. Rotation of the fragments during progressive deformation produced a preferred orientation of poles to the slip...