Field-observed phenomena of seismic liquefaction and subsidence during the 2008 Wenchuan earthquake in China

Author:

Huang Yu,Jiang Ximiao

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Water Science and Technology

Reference11 articles.

1. China Earthquake Administration (2008a) Analysis of the cause of the M8.0 Wenchuan earthquake. http://www.cea.gov.cn/manage/html/8a8587881632fa5c0116674a018300cf/content/08_05/30/1212119940937.html Last accessed 28/10/2009 (in Chinese)

2. China Earthquake Administration (2008b) Seismic intensity map of the M8.0 Wenchuan earthquake. http://www.cea.gov.cn/manage/html/8a8587881632fa5c0116674a018300cf/_content/08_08/29/1219979564089.html Last accessed 28/10/2009 (in Chinese)

3. Chu DB, Stewart JP, Lee S, Tsai JS, Lin PS, Chu BL, Seed RB, Hsu SC, Yu MS, Wang MCH (2004) Documentation of soil conditions at liquefaction and non-liquefaction sites from 1999 Chi–Chi (Taiwan) earthquake. Soil Dyn Earthq Eng 24(9–10):647–657

4. Cundy AB, Kortekaas S, Dewez T, Stewart IS, Collins PEF, Croudace IW, Maroukian H, Papanastassiou D, Gaki-Papanastassiou P, Pavlopoulos K, Dawsonb A (2000) Coastal wetlands as recorders of earthquake subsidence in the Aegean: a case study of the 1894 Gulf of Atalanti earthquakes, central Greece. Mar Geol 170(3):3–26

5. Evans MD, Zhou S (1995) Liquefaction behavior of sand-gravel composites. J Geotech Eng ASCE 121(3):287–298

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