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Department of Earth Science, Geodynamics Group

Department of Earth Science, Geodynamics Group. Department of Earth Science, Geodynamics Group. www.geo.uib.no. Svalbard earthquake of 21 Feb. 2008 (M=6.0). K. Atakan, L. Ottemöller, M. Raeesi and J. Havskov. Department of Earth Science, Geodynamics Group.

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Department of Earth Science, Geodynamics Group

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  1. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no Svalbard earthquake of 21 Feb. 2008 (M=6.0) K. Atakan, L. Ottemöller, M. Raeesi and J. Havskov

  2. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no Jordskjelvet på Svalbard 21 februar 2008 (M=6.0)

  3. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no Svalbard earthquake (21.feb.2008) recorded at Tromsø station

  4. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no Svalbard earthquake (21.feb. 2008) record at Kings Bay (Spitsbergen).

  5. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no Svalbard earthquake (21.feb. 2008) record at Bjørnøya station.

  6. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no Svalbard earthquake (21.feb. 2008) record at Kongsberg station.

  7. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no

  8. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no The earthquake occurred likely between the Billedfjord and Lomfjorden faults. More than 2000 aftershocks are recorded.

  9. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no More than 200 aftershocks are located.

  10. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no MT-inversion on regional stations (depth fixed to 15 km)

  11. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no MT-inversion on local stations

  12. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no Focal mechanism based on the first motion polarities (left) and based on the slip inversion (right)

  13. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no

  14. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no (Ingolfsson, 2007)

  15. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no The focal mechanism is compatible with E-W oriented maximum horizontal compression. Fault rupture area is roughly 9 x 11 km. (Ingolfsson, 2007)

  16. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no (Breivik et al., 2005)

  17. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no (Breivik et al., 2005)

  18. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no (Breivik et al., 2005)

  19. Department of Earth Science, Geodynamics Group Norsk Nasjonalt Seismisk Nettverk (NNSN) Department of Earth Science, Geodynamics Group www.geo.uib.no Institutt for geovitenskap, Universitetet i Bergen

  20. Department of Earth Science, Geodynamics Group Department of Earth Science, Geodynamics Group www.geo.uib.no Thank you for your attention!

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