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K. Atakan Dept. of Earth Science University of Bergen Allégt.41, 5007 Bergen

Fault rupture process and its influence on the development of the deformation zone: a perspective from recent seismological and paleoseismological data. K. Atakan Dept. of Earth Science University of Bergen Allégt.41, 5007 Bergen E-mail: atakan@geo.uib.no.

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K. Atakan Dept. of Earth Science University of Bergen Allégt.41, 5007 Bergen

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  1. Fault rupture process and its influence on the development of the deformation zone: a perspective from recent seismological and paleoseismological data K. Atakan Dept. of Earth Science University of Bergen Allégt.41, 5007 Bergen E-mail: atakan@geo.uib.no

  2. The present study has largely benefited from the results of the European Project RELIEF (EC-EVG1-CT-2002-00069)

  3. modified from Herece and Akay, 2003 andfrom Akyuz et al., 2000

  4. Pucci et al., 2004

  5. N

  6. CIN Site De Martini et al., 2004

  7. CH - Site De Martini et al., 2004

  8. Pucci et al., 2004

  9. N fault trace

  10. ridge hingeline fault trace N A A’ Pucci et al., 2004

  11. N B 1999 ruptures warp hingline N B’

  12. N ridge hingeline fault trace

  13. Man Site De Martini et al., 2004

  14. N N

  15. Pucci et al., 2004

  16. Pucci et al., 2004

  17. northward migration of the active fault

  18. Kay Site De Martini et al., 2004

  19. Pucci et al., 2004

  20. 4.5 km

  21. N Slip rate from stream deflections Pucci et al., 2004

  22. Pucci et al., 2004

  23. 135 m

  24. 900 m 300 m Slip rate from terrace offset

  25. Pucci et al., 2004

  26. 900 m 300 m

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