1-20 OF 206 RESULTS FOR

Tabas earthquake 1978

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 December 1979
Bulletin of the Seismological Society of America (1979) 69 (6): 1861–1887.
...’; a seismotectonic discussion , Geol. Surv. Iran 40 , 203 - 227 . Berberian M. (1977b) . Contribution to the seismotectonics of Iran (part III) , Geol. Min. Surv. Iran 40 , 279 pp. Berberian M. (1979a) . Tabas-e-Golshan (Iran) catastrophic earthquake of 16 September 1978...
Journal Article
Published: 01 February 1994
Bulletin of the Seismological Society of America (1994) 84 (1): 31–46.
...Chandan K. Saikia Abstract We have examined the adequacy of the published KS3 and L1 slip distribution models developed for the M S = 7.4 16 September 1978 Tabas earthquake (Hartzell and Mendoza, 1991) by modeling the high-frequency accelerograms recorded at Dayhook, Boshrooyeh, and Tabas stations...
Journal Article
Published: 01 April 1991
Bulletin of the Seismological Society of America (1991) 81 (2): 305–331.
...Stephen Hartzell; Carlos Mendoza Abstract An iterative least-squares technique is used to simultaneously invert the strong-motion records and teleseismic P waveforms for the 1978 Tabas, Iran, earthquake to deduce the rupture history. The method solves for both slip amplitudes and rupture times...
Journal Article
Published: 01 February 1988
Bulletin of the Seismological Society of America (1988) 78 (1): 142–171.
...Jafar Shoja-Taheri; John G. Anderson Abstract The 1978 Tabas, Iran, earthquake ( M s = 7.4) was registered on 11 accelerograph stations, with source distances ranging from 3 to 350 km and corresponding recorded peak accelerations ranging from 0.95 down to 0.01 g, respectively. At least four...
Journal Article
Published: 01 May 1986
Earthquake Spectra (1986) 2 (3): 635–651.
...Mansour Niazi, M.EERI Three triaxial sets of accelerograms recorded in the near source region (within 50 km epicentral distance) of the September 16, 1978, Tabas earthquake (M s 7.4 -7.7) are of great engineering importance. The distances of the recording sites from the nearest approach...
Journal Article
Published: 01 February 1983
Bulletin of the Seismological Society of America (1983) 73 (1): 315–320.
.... Scholz C. H. Soufleris C. (1979) . Mechanism of the main shock and the aftershock study of the Tabas-e-Golshan (Iran) earthquake of September 16, 1978: preliminary report , Bull. Seism. Soc. Am. 69 , 1851...
Journal Article
Published: 01 December 1979
Bulletin of the Seismological Society of America (1979) 69 (6): 1851–1859.
...M. Berberian; I. Asudeh; R. G. Bilham; C. H. Scholz; C. Soufleris abstract Aftershocks of the Tabas-e-Golshan earthquake ( M s = 7.7) of September 16, 1978 were recorded with a local network of portable seismometers. The main shock produced a discontinuous series of surface ruptures extending 85 km...
Journal Article
Published: 01 August 1981
Bulletin of the Seismological Society of America (1981) 71 (4): 1201–1213.
...Mansour Niazi; Hiroo Kanamori abstract The teleseismic records of three strong earthquakes which inflicted heavy damage and loss of many thousands of lives in northeastern Iran during 1978 and 1979 are analyzed. The observed R 2 and R 3 phases of the 16 September 1978 Tabas earthquake across...
Journal Article
Published: 01 February 1999
Bulletin of the Seismological Society of America (1999) 89 (1): 120–139.
... reverse fault systems. The two pairs of earthquakes may have ruptured different faults in each segment, similar to the 1971 and 1994 San Fernando, California, earthquakes. The 1978 Tabas reversefault earthquake was preceded by the 1968 Ferdows earthquake, part of the Dasht-e-Bayaz sequence. The North...
Image
Various measures of 5%-damped relative response spectral displacements ( SD...
Published: 01 August 2010
Figure 1. Various measures of 5%-damped relative response spectral displacements ( SDs ) for the horizontal-component recordings of the 1978 Tabas earthquake at the Tabas station. Although hard to see in the graph, RotI50 is almost equal to RotD100 for periods from 1.7 to 3.3 sec.
Image
The response of a representative handheld device compared to the reference ...
Published: 01 May 2014
Figure 6. The response of a representative handheld device compared to the reference accelerometer during ST-2. Input ground motion: 1978 Tabas, Iran, earthquake.
Image
The spectral values for two records of 16 September <b>1978</b>  M  w  7.4 <b>Tabas</b> e...
Published: 01 December 2012
Figure 9. The spectral values for two records of 16 September 1978 M w  7.4 Tabas earthquake (left) and event with 14 March 1998 M w  6.9 (right).
Image
Spectral predictions derived from our proposed model corresponding to the 1...
Published: 02 April 2019
Figure 13. Spectral predictions derived from our proposed model corresponding to the 1978 Tabas earthquake (black squares) and the 2012 Ahar–Varzaghan earthquakes (gray circles) for (a) PGA and (b–d) SA ( T = 0.4 , 1.5, and 8 s). Dashed curves show the ± 1 σ bounds
Image
5%-damped acceleration response spectra recorded by the reference accelerom...
Published: 01 May 2014
record: 1978 Tabas, Iran, earthquake.
Image
Acceleration time histories and 5%-damped acceleration response spectra obt...
Published: 01 May 2014
Figure 17. Acceleration time histories and 5%-damped acceleration response spectra obtained from phones with frictional covers allowed to move freely on the shake table compared to the reference during the 1978 Tabas, Iran, earthquake motion in ST-2 (only showing the horizontal component
Image
Omni‐spectrum ( OS ) over a range of periods from 0.01 to 10 s. The ground ...
Published: 15 April 2014
Figure 5. Omni‐spectrum ( OS ) over a range of periods from 0.01 to 10 s. The ground motion is from the PEER NGA Ground‐Motion Database with record sequence number 143 (Tabas station, Iran, 16 September 1978 earthquake). In the legend, periods are shown in seconds.
Image
Ratios for the  OS  of the ground motion from the PEER  NGA  Ground‐Motion ...
Published: 15 April 2014
Figure 6. Ratios for the OS of the ground motion from the PEER NGA Ground‐Motion Database with record sequence number 143 (Tabas station, Iran, 16 September 1978 earthquake). The ratio is the spectral value over RotD50 for all nonredundant orientations, and periods range from 0.01 to 10 s.
Image
Percentage difference for the spectra computed by the projected envelope an...
Published: 15 April 2014
September 1978 earthquake). The color version of this figure is available only in the electronic edition.
Image
A pseudospectral acceleration response trace generated by an oscillator wit...
Published: 15 April 2014
, 16 September 1978 earthquake). The color version of this figure is available only in the electronic edition.
Image
Characteristics of the <b>earthquake</b> ground motion histories                 S...
Published: 01 August 2015
Table 4 Characteristics of the earthquake ground motion histories SL no. Earthquake Year Richter magnitude Epicentral distance (km) PGA (g) PGV (cm/s) 1 Tabas 1978 7.4 1.2 0.922 108.0 2 Tabas 1978 7.4 1.2 0.958 103.8 3 Loma Prieta 1989 7.0 3.5