Počet záznamů: 1  

Tracing of travelling of stress deformation waves after the Tohoku earthquake

  1. 1.
    0433794 - ÚGN 2015 AU eng A - Abstrakt
    Kalenda, Pavel - Holub, Karel - Rušajová, Jana - Neumann, L.
    Tracing of travelling of stress deformation waves after the Tohoku earthquake.
    Earth on the Edge: Science for a Sustainable Planet Proceedings of the IAG General Assembly, Melbourne, Australia - 2011. Vol. 25. Melbourne: Springer eBooks - SpringerLink (Online service), 2014 - (Rizos, C.; Willis, P.). ISBN 978-3-642-37222-3.
    [IUGG General Assembly 2011 /25./ - Earth on the Edge: Science for a Sustainable Planet. 27.06.2011-08.07.2011, Melbourne]
    Institucionální podpora: RVO:68145535
    Klíčová slova: deformation waves * Tohoku earthquake * microseisms
    Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země
    http://www.iugg.org/assemblies/2011melbourne/2011%20GA%20Melbourne%20CR_PART%20I.pdf

    The deformation waves, which were created during the strongest earthquakes, were traced on their way around the globe. These deformation waves follow the focal mechanisms and start after the mainshocks. The deformation waves after the Chile earthquake on February 27, 2010 (M=8,8´) and the Mentawai earthquake (Indonesia) on October 25, 2010 (M=7,7) used the global tectonic structures with NW-SE orientations and they spread mostly to the west - northwest. On the other hand, two deformation waves were created after the Tohoku earthquake on March 11, 2011 (M=7,3, M=9). The first, a weaker deformation wave spread to the west from Honshu and the second travelled to the north and through the north pole to Greenland and Europe.
    Trvalý link: http://hdl.handle.net/11104/0237947

     
    Název souboruStaženoVelikostKomentářVerzePřístup
    UGN_0433794.pdf1179.2 KBVydavatelský postprintpovolen
     
Počet záznamů: 1  

  Tyto stránky využívají soubory cookies, které usnadňují jejich prohlížení. Další informace o tom jak používáme cookies.