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Publications tagged with [earthquake epicenter]

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<p>A considerable number of damaging earthquakes in Greece, have produced a variety of macroseismic effects to both built and natural environment. After a strong earthquake, rotational effects have been observed mainly on free-standing columns, statues, chimneys, ...
Reference: Second European Conference on Earthquake Engineering and Seismology, Istanbul Aug. 25-29, 2014
Tectonic deformation from the 2010 Maule (Chile) Mw 8.8 earthquakeincluded both uplift and subsidence along about 470 km of the central Chilean coast. In the south, deformation included as much as 3 m of uplift of the Arauco Peninsula, which produced emergent ...
Reference: Earthquake Spectra, Volume 28, No. S1, pages S39–S54, June 2012; 2012, Earthquake Engineering Research Institute
A devastating earthquake hit the Tohoku and Kanto regions of Japan on 11 March 2011, causing extensive damage to life and property as a result of large-scale tsunami and damage to nuclear power plants. Many slope failures occurred in hilly areas, such as in ...
Reference: NZSEE Annual Technical Conference & AGM, 13-15 April 2012, Christchurch
On 22 February 2011 the Mw6.2 Christchurch earthquake occurred with an epicentre less than 10 km from the Christchurch Central Business District (CBD) on an unknown buried fault at the edge of the city. The majority of damage was a result of lateral spreading ...
Reference: BULLETIN OF THE NEW ZEALAND SOCIETY FOR EARTHQUAKE ENGINEERING, Vol. 44, No. 4, December 2011
 
On Saturday, February 27, 2010, at 03:34 a.m. local time (06:34:14 UTC), an Mw 8.8 earthquake struck the central south region of Chile, affecting an area with a population exceeding eight million people, including 6.1M, 0.8M, and 0.9M in the urban areas around ...
Reference: EERI Special Earthquake Report — June 2010
This thesis deals with the model accuracy for seismic design of immersed tunnels, like the proposed underwater artery in Thessaloniki, Greece. The soil response to seismic waves is analysed in the frequency domain by means of the domain transformation method ...
Reference: MASTER’S THESIS THE SCHOOL OF CIVIL ENGINEERING, MASTER OF SCIENCE IN CIVIL AND STRUCTURAL ENGINEERING, AALBORG UNIVERSITY, 2008
In this paper is shown that the earthquake's true size and tsunami potential can be determined using GlobalPositioning System (GPS) data up to only 15 min after earthquake initiation, by tracking the mean displacement of the Earth's surface associated with ...
Reference: GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L11309, 2006
 
A magnitude 6.6 (Ms) earthquake struck the city of Bam in southeast Iran at 5:26:52 AM (local time) on Friday, December 26, 2003. The city’s population was about 90,000, with 200,000 total residents in the greater Bam area. The U.N. Office for the Coordination ...
Reference: EERI Special Earthquake Report — April 2004