1974 Zhaotong earthquake
  | |
| Date | 10 May 1974 |
|---|---|
| Magnitude | 7.1 Ms |
| Depth | 14 km (8.7 mi) [1] |
| Epicenter | 28°14′N 104°01′E / 28.24°N 104.01°ECoordinates: 28°14′N 104°01′E / 28.24°N 104.01°E [2] |
| Areas affected | China, Yunnan, Sichuan |
| Max. intensity | IX (Violent) |
| Casualties | 1,641–20,000 [2][3] |
The 1974 Zhaotong earthquake occurred at 19:25 UTC on 10 May. It had a magnitude that was measured at 7.0 on the moment magnitude scale[4] and 7.1 on the surface wave magnitude scale. It had a maximum perceived intensity of IX (Violent) on the Mercalli intensity scale. The epicenter was located in Zhaotong prefecture in Yunnan province and it caused between 1,641 and 20,000 deaths.
Earthquake
The earthquake has been ascribed to slip on a thrust fault trending north-south with a dip of 60° to the east, from geodetic data analysis.[5] It has also been interpreted to result from strike-slip faulting along a steeply-dipping NW-SE trending fault.[4] The isoseismal lines for the earthquake were poorly defined, due to variations both in topography and ground conditions.[1]
The earthquake consisted of more than ten separate sub-events. The sequence began with a few shocks in the first two to three seconds with magnitudes less than 5. These were followed by several shocks approaching magnitude 7 over a period of about a minute. The areal distribution of the individual shocks showed no progression along the fault plane as would be expected with a propagating fracture.[6]
The earthquake triggered many landslides in the epicentral area. The bedrock geology in the area contains rocks of almost all ages from Neoproterozoic through to Quaternary. Landslides were mainly confined to areas that experienced intensities of VII or greater and had slopes of moderate dip (26°–45°). In all but one case, the landslides involved Quaternary material, the exception being a slide that was controlled by bedding planes in a Permian limestone. Rock avalanches occurred on steeper slopes, particularly affecting jointed and weathered Permian limestone and Triassic sandstone/shale sequences.[7]
Damage
An area of about 400,000 square kilometres was affected by the earthquake. 28,000 houses collapsed and a further 38,000 were damaged. Houses with wooden frames in the epicentral area remained undamaged.[8] The number of deaths reported varies from 1,641 to 20,000[2][3] with a further 1,600 injured.
The largest landslide formed a dam up to 30 m high across the Yangtze River, turning the valley above it into a lake.[8]
References
- 1 2 Hu, Y.; Liu S.C. & Dong W. (1996). "Earthquakes in China". Earthquake Engineering. Taylor & Francis. pp. 107–108. ISBN 9780419205906. Retrieved 17 July 2012.
- 1 2 3 National Geophysical Data Center. "Comments for the Significant Earthquake". Retrieved 17 July 2012.
- 1 2 Utsu, T. R. (2002), "A List of Deadly Earthquakes in the World: 1500–2000", International Handbook of Earthquake & Engineering Seismology, Part A, Volume 81A (First ed.), Academic Press, p. 708, ISBN 978-0124406520
- 1 2 Zhuo, Y.; Kanamori H. (1987). "Regional variation of the short-period (1 to 10 second) source spectrum" (PDF). Bulletin of the Seismological Society of America. Seismological Society of America. 77 (2): 514–529. Retrieved 18 July 2012.
- ↑ Zhu, C.-N.; Chen C.-Z. (1976). "The Rupture Mechanism of the Zhaotong earthquake of 1974 in Yunnan Province". Chinese Journal of Geophysics. 19 (4): abstract only. Retrieved 17 July 2012.
- ↑ Tseng, J.S.; Shi J.S. (1978). "Source multiplicity of the main shock of the Yong Shan-Da Guan Yunnan Earthquake of May 10, 1974". Acta Geophysica Sinica. 21: 160–173. Retrieved 18 July 2012.
- ↑ Chen, X.L.; Zhou Q., Ran H. & Dong R. (2012). "Earthquake-triggered landslides in southwest China" (PDF). Natural Hazards Earth System Science. Copernicus Publications. 12: 351–363. doi:10.5194/nhess-12-351-2012. Retrieved 17 July 2012.
- 1 2 Museum of Earthquakes. "Earthquakes in China: Typical earthquakes". Computer Network Information Center of Chinese Academy of Sciences. Retrieved 22 July 2012.