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Shandan earthquake 1954

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Topographic profiles measured across the <span class="search-highlight">1954</span> <span class="search-highlight">Shandan</span> <span class="search-highlight">earthquake</span> surface-ru...
Published: 01 April 2010
Figure 14. Topographic profiles measured across the 1954 Shandan earthquake surface-rupture zone (see Fig.  13 for profile locations). Topographic profiles D, F, H, I, and J have slope breaks that record an older earthquake (upper gentle scarp) in addition to the 1954 Shandan earthquake
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Distribution of the <span class="search-highlight">1954</span> <span class="search-highlight">Shandan</span> <span class="search-highlight">earthquake</span> surface-rupture zone and simpli...
Published: 01 April 2010
Figure 13. Distribution of the 1954 Shandan earthquake surface-rupture zone and simplified geology along the Baode fault (see Fig.  2 for location). The inset map (lower right) shows isoseismal lines for the 1954 Shandan earthquake. The 1954 rupture is shown in bold lines.
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Isoseismal map of the <span class="search-highlight">Shandan</span> <span class="search-highlight">earthquake</span> in <span class="search-highlight">1954</span> (after  Gu et al., 1989 )....
Published: 01 March 2002
Figure 4. Isoseismal map of the Shandan earthquake in 1954 (after Gu et al., 1989 ).
Journal Article
Published: 01 April 2010
Bulletin of the Seismological Society of America (2010) 100 (2): 541–561.
...Figure 14. Topographic profiles measured across the 1954 Shandan earthquake surface-rupture zone (see Fig.  13 for profile locations). Topographic profiles D, F, H, I, and J have slope breaks that record an older earthquake (upper gentle scarp) in addition to the 1954 Shandan earthquake...
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Journal Article
Published: 04 August 2015
Bulletin of the Seismological Society of America (2015) 105 (5): 2724–2735.
... between the active faults around northeastern Tibet during the earthquake process even though they were separated by hundreds of kilometers. Numerical results also suggest that the 1954 M ∼7.2 Shandan earthquake and the 1990 M ∼6.2 Tianzhu earthquake could have been triggered because the Coulomb failure...
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View north at shutter ridge and right-lateral gully offset along the Baode ...
Published: 01 April 2010
Figure 15. View north at shutter ridge and right-lateral gully offset along the Baode fault during the 1954 Shandan earthquake. South-facing fault scarp is toward the camera and is higher to the left of the gully and lower to the right, consistent with a predominantly right-lateral slip
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Accumulation of Coulomb failure stress around epicenters of the strong eart...
Published: 04 August 2015
on earthquake of (a) the 1927 Gulang event, (b) the 1932 Changma event, (c) the 1954 Shandan event, and (d) 1990 Tianzhu event. All the stress is at a depth of 5 km with the effective coefficient of friction of 0.4. The crustal viscosities are from the solid lines in Figure  2b .
Journal Article
Published: 01 March 2002
Bulletin of the Seismological Society of America (2002) 92 (2): 783–793.
...Figure 4. Isoseismal map of the Shandan earthquake in 1954 (after Gu et al., 1989 ). ...
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Seismic Parameters for Historical <span class="search-highlight">Earthquakes</span> along the Hexi Corridor      ...
Published: 01 April 2010
7.6–7.7 7.7 6.9 5 †† Changma 25-12-1932 X 7.6 h 2.3/15 h 6.2 149 7.6 7.7 7.1–7.2 6 Shandan 11-2-1954 X 7.3 h 1.2/9 h 1.5 5.1 6.0 6.4 6.9 * Department of Earthquake Disaster Prevention, CEA (1995) . † Earthquake magnitude M is estimated by empirical equation
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Seismic Parameters for Historical <span class="search-highlight">Earthquakes</span> along the Hexi Corridor      ...
Published: 01 April 2010
7.6–7.7 7.7 6.9 5 †† Changma 25-12-1932 X 7.6 h 2.3/15 h 6.2 149 7.6 7.7 7.1–7.2 6 Shandan 11-2-1954 X 7.3 h 1.2/9 h 1.5 5.1 6.0 6.4 6.9 * Department of Earthquake Disaster Prevention, CEA (1995) . † Earthquake magnitude M is estimated by empirical equation
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Seismic Parameters for Historical <span class="search-highlight">Earthquakes</span> along the Hexi Corridor      ...
Published: 01 April 2010
7.6–7.7 7.7 6.9 5 †† Changma 25-12-1932 X 7.6 h 2.3/15 h 6.2 149 7.6 7.7 7.1–7.2 6 Shandan 11-2-1954 X 7.3 h 1.2/9 h 1.5 5.1 6.0 6.4 6.9 * Department of Earthquake Disaster Prevention, CEA (1995) . † Earthquake magnitude M is estimated by empirical equation
Image
Seismic Parameters for Historical <span class="search-highlight">Earthquakes</span> along the Hexi Corridor      ...
Published: 01 April 2010
7.6–7.7 7.7 6.9 5 †† Changma 25-12-1932 X 7.6 h 2.3/15 h 6.2 149 7.6 7.7 7.1–7.2 6 Shandan 11-2-1954 X 7.3 h 1.2/9 h 1.5 5.1 6.0 6.4 6.9 * Department of Earthquake Disaster Prevention, CEA (1995) . † Earthquake magnitude M is estimated by empirical equation
Image
Seismic Parameters for Historical <span class="search-highlight">Earthquakes</span> along the Hexi Corridor      ...
Published: 01 April 2010
7.6–7.7 7.7 6.9 5 †† Changma 25-12-1932 X 7.6 h 2.3/15 h 6.2 149 7.6 7.7 7.1–7.2 6 Shandan 11-2-1954 X 7.3 h 1.2/9 h 1.5 5.1 6.0 6.4 6.9 * Department of Earthquake Disaster Prevention, CEA (1995) . † Earthquake magnitude M is estimated by empirical equation
Image
Seismic Parameters for Historical <span class="search-highlight">Earthquakes</span> along the Hexi Corridor      ...
Published: 01 April 2010
7.6–7.7 7.7 6.9 5 †† Changma 25-12-1932 X 7.6 h 2.3/15 h 6.2 149 7.6 7.7 7.1–7.2 6 Shandan 11-2-1954 X 7.3 h 1.2/9 h 1.5 5.1 6.0 6.4 6.9 * Department of Earthquake Disaster Prevention, CEA (1995) . † Earthquake magnitude M is estimated by empirical equation
Journal Article
Published: 14 August 2024
Seismological Research Letters (2025) 96 (1): 65–77.
... et al. , 2017 ). Many strong earthquakes have occurred in the region during the past decades, such as the 1920 M s  8.5 Haiyuan, 1927 M s  8.0 Gulang, 1954 M s  7.2 Shandan, 1986 M s  6.4 Menyuan, and 2016 M s  6.4 Menyuan earthquakes. The 2022 Menyuan...
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Journal Article
Published: 17 January 2024
Bulletin of the Seismological Society of America (2024) 114 (3): 1481–1506.
... been reported in the region, mainly occurring along the Lenglongling fault. Strong earthquakes in the region mainly include the 1927 M w  7.7 Gulang, 1954 M w  7.0 Shandan, 1986 M w  6.3 Menyuan, 2003 M w  5.9 Minle‐Shandan, and 2016 M w  6.1 Menyuan earthquakes...
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Journal Article
Published: 30 March 2023
Seismological Research Letters (2023) 94 (4): 1747–1760.
... ), 1927 M w  8.0 Gulang earthquake ( Deng et al. , 1986 ; Guo et al. , 2020 ), 1954 M 7.0 Minqin earthquake, 1954 M  7.3 Shandan earthquake, and 1986 M w  6.0 and 2016 M w  5.9 Menyuan earthquakes ( Pan et al. , 2022 ). Figure 1. Tectonic setting of the 2022 M w...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 12 December 2019
Lithosphere (2020) 12 (1): 19–39.
... and Yin, 2009 ). Several large earthquakes occurred during and after the 20th century on these active faults, including the 1932 Ms 7.6 Changma earthquake, the 1954 Ms 7¼ Shandan earthquake ( Tapponnier and Molnar, 1977 ; Deng, 1984 ), and the 2002 Ms 5.9 Yumen earthquake ( He et al., 2004 ) ( Fig. 1...
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Journal Article
Published: 01 February 2007
Bulletin of the Seismological Society of America (2007) 97 (1B): 14–34.
... of China Earthquake Administration, 1990 ; Committee for Chinese Earthquake Bulletin, 1990 ). This earthquake was the biggest event in Gansu province since the 1954 Shandan earthquake ( M s ∼7.3). It caused severe damage (intensity VIII) in villages along a 27-km-long stretch of the Haiyuan fault...
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