1931 Fuyun earthquake
  | |
| UTC time | 1931-08-10 21:18:45 |
|---|---|
| ISC event | 906933 |
| USGS-ANSS | ComCat |
| Local date | August 11, 1931 |
| Local time | 05:18:45 |
| Magnitude | Mw 8.0 |
| Depth | 20 km[1] |
| Epicenter | 46°48′N 89°54′E / 46.8°N 89.9°E |
| Max. intensity | MMI XI (Extreme)[2] |
| Casualties | 10,000 dead[2][3] |
The 1931 Fuyun earthquake (富蕴地震) occurred on August 10 at 21:18 UTC.[4] The epicenter was near Fuyun County of northern Xinjiang, China. It was a Mw 8.0 earthquake[5] and had a surface rupture of 171 km[1] with a maximal horizontal displacement of 14 m[6] along the Koktokay-Ertai fault zone (可可托海-二台断裂带).[7] The Koktokay-Ertai fault has a slip rate of 4±2 mm per year.[8] The rupture of this earthquake was caused by right-lateral strike-slip movement with normal component.[9] The rupture is well preserved and becomes one of the main features of the Koktokay National Geopark (可可托海国家地质公园) located in Koktokay.[10]
See also
[edit]References
[edit]- ^ Jump up to: a b Vergnolle, Mathilde; Pollitz, Fred; Calais, Eric (2003), "Constraints on the viscosity of the continental crust and mantle from GPS measurements and postseismic deformation models in western Mongolia", Journal of Geophysical Research: Solid Earth, 108 (B10): 2502, Bibcode:2003JGRB..108.2502V, doi:10.1029/2002JB002374
- ^ Jump up to: a b National Geophysical Data Center / WorldSignificant Earthquake Information Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information (1972). "Significant Earthquake Information". NOAA National Centers for Environmental Information. doi:10.7289/V5TD9V7K. Retrieved 28 March 2022.
- ^ "Earthquakes with 1,000 or More Deaths since 1900". Earthquake.usgs.gov. Archived from the original on 2013-01-14. Retrieved 2011-10-22.
- ^ "Magnitude 8 and Greater Earthquakes Since 1900". Earthquake.usgs.gov. Archived from the original on 2016-04-14. Retrieved 2011-10-22.
- ^ Pollitz, F.; Vergnolle, M.; Calais, E. (2003). "Fault interaction and stress triggering of twentieth century earthquakes in Mongolia" (PDF). Journal of Geophysical Research. 108 (B10): 2503. Bibcode:2003JGRB..108.2503P. doi:10.1029/2002JB002375. Archived from the original (PDF) on 2011-07-21. Retrieved 2010-07-24.
- ^ "地震知识-中国科学院地球环境研究所". Ieexa.cas.cn. 2008-06-04. Archived from the original on 2020-11-07. Retrieved 2011-10-22.
- ^ Shi, Lanbin; Lin, Chuanyong; Zhang, Xiaoou; Chen, Xiaode; Bai, Meixiang (1997). "Pseudotachylytes from the Koktokay-Ertai fault zone, Xinjiang, China, and their seismogeologic implications". Science in China Series D: Earth Sciences. 40 (2): 189–196. Bibcode:1997ScChD..40..189S. doi:10.1007/BF02878378. S2CID 130570844.
- ^ "中国科技论文在线". www.paper.edu.cn.[permanent dead link]
- ^ Awata, Y; Fu, B; Zhang, Z (2008). "Re-investigation of the Geometry and Slip Distribution of the 1931 Fuyun Surface". American Geophysical Union, Fall Meeting. 41: T41A–1930. Bibcode:2008AGUFM.T41A1930A.
- ^ "中国公众科技网". Special.cpst.net.cn. Archived from the original on 2011-11-24. Retrieved 2011-10-22.
External links
[edit]- The International Seismological Centre has a bibliography and/or authoritative data for this event.
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