Implications of paleoseismology in seismic hazard analysis in NW Crete and Kythira strait (Greece)

PDF (English)
Publiée : Jan 1, 2001
DOI : https://doi.org/10.12681/bgsg.17244
C. ANDREOU
University of Athens, Faculty of Geology Dept of Dynamic Tectonic Applied Geology
V. MOUSLOPOULOU
University of Athens, Faculty of Geology Dept of Dynamic Tectonic Applied Geology
I. FOUNTOULIS
University of Athens, Faculty of Geology Dept of Dynamic Tectonic Applied Geology
Κ. ATAKAN
Institute of Solid Earth Physics, Univ. of Bergen
Résumé

The scope of this paper is to study how geological data contribute to hazard analysis and the extent to which they can be incorporated in the existing hazard models. For this reason the study area was divided into area source zones and the paleoseismological data collected and studied on the Kera fault zone, in Chania, Crete, were taken into account. The seismic hazard was calculated with CRISIS99, using a combination of the Poissonian and the characteristic earthquake model. The data from the Kera fault affect slightly the calculation of seismic hazard. It is suggested that more paleoseismological data and a good attenuation relationship for the area, would lead to the development of hazard models capable to incorporate geological information and it would improve the quality of seismic hazard analysis.

Article Details
  • Rubrique
  • Seismology
Creative Commons License

Ce travail est disponible sous licence Creative Commons Attribution - Pas d’Utilisation Commerciale 4.0 International.

Authors who publish with this journal agree to the following terms:

Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution Non-Commercial License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.

Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g. post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal. Authors are permitted and encouraged to post their work online (preferably in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work.

Téléchargements
Les données relatives au téléchargement ne sont pas encore disponibles.
Références
AMBRASSEYS, Ν. Ν., 1981. On the long term seismicity of the Hellenic arc. Boll. Teor. Geof. Appi. XXIII, 355-359.
ANDREOU C, 2000. Seismic Hazard Analysis Of Western Crete And Kythira Strait, Institute of Solid Earth Physics, University of Bergen, pp. 1-180.
HAVSKOV J., 1999. The SEISAN earthquake analysis software for the IBM PC and SUN, institute of Solid Earth Physics, university of Bergen.
LYBERIS, N., ANGELIER, J. et al., 1982. Active deformation of a segment of arc: the strait of Kythira, Hellenic arc GREECE. Journal of Structural Geology, vol 4, No 3, 299-311.
MAKROPOULOS, K. and BURTON W., 1981. A catalogue of seismicity in Greece and adjacent areas. J.R. Astr. Soc, 65, pp. 741-762.
MOUSLOPOULOU et al., 2000. Paleoseismological investigations along the Kera Fault Zone, Western Crete: Implications for seismic hazard assessment, pp. 1-130.
ORDAZ, M (1991). CRISIS 1999. Brief description of program CRISIS. Institute of Solid Earth Physics, University of Bergen, Norway, Internal Report, 16p.
PAPADOPOULOS G.A. and VASSILOPOULOU, Α., 1998. Historical and Archaeological evidence of earthquakes and Tsunamis felt in the Kythira strait, Greece. Institute of Geodynamics, NOA publication No 9.
Pers. com. H. BUNGUM. Numerical modeling of fault activity, mom_slip and mom_rate programs.
SADIGH et. al. (1997). Attenuation Relationships for Shallow Crustal Earthquakes Based on California Strong Motion Data, Seismological Research Letters, 68, January /February, 1997).
THEODOULIDES,N. and, PAPAZACHOS, B., 1992. Dependence of strong ground motion on magnitude, distance, site geology and macroseismic intensity for shallow earthquakes in Greece. Soil Dyn. & Earth. Engn., 13,317-343.
WELLS, D.L. and COPPERSMITH, K.J., 1994. Empirical relationships among magnitude, rupture length, rupture area, and surface displacement. Bull. Seism. Soc. Am., 84, 974-1784.
YOUNGS, R. R. and K.J. COPPERSMITH, 1985. Implications of fault slip rates and earthquake recurrence models to probabilistic seismic hazard estimates. Bull. Seism. Soc. Am., 75, 939-964.
Articles les plus lus par le même auteur ou la même autrice