Evaluation of The Seismic Hazard in The Marmara Region (Turkey) Based on Updated Databases
The increase in the wealth of information on the seismotectonic structure of the Marmara region after two devastating earthquakes (<b>M</b>7.6 Izmit and <b>M</b>7.2 Duzce events) in the year 1999 opened the way for the reassessment of the probabilistic seismic hazard in the l...
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doaj-06cf043a308f4cc7a28c616adff206be2020-11-25T01:39:57ZengMDPI AGGeosciences2076-32632019-11-0191248910.3390/geosciences9120489geosciences9120489Evaluation of The Seismic Hazard in The Marmara Region (Turkey) Based on Updated DatabasesKarin Şeşetyan0Mine Betül Demircioğlu Tümsa1Aybige Akinci2Department of Earthquake Engineering, Kandilli Observatory and Earthquake Research Institute, Boğaziçi University, Cengelkoy, 34684 Istanbul, TurkeyMD Consulting Engineers, Caferağa Mah., Keresteci Aziz Sk. No:5/33, Kadikoy, 34710 Istanbul, TurkeyIstituto Nazionale di Geofisica e Vulcanalogia, Via di Vigna Murata 605, 00143 Rome, ItalyThe increase in the wealth of information on the seismotectonic structure of the Marmara region after two devastating earthquakes (<b>M</b>7.6 Izmit and <b>M</b>7.2 Duzce events) in the year 1999 opened the way for the reassessment of the probabilistic seismic hazard in the light of new datasets. In this connection, the most recent findings and outputs of different national and international projects concerning seismicity and fault characterization in terms of geometric and kinematic properties are exploited in the present study to build an updated seismic hazard model. A revised fault segmentation model, alternative earthquake rupture models under a Poisson and renewal assumptions, as well as recently derived global and regional ground motion prediction equations (GMPEs) are put together in the present model to assess the seismic hazard in the region. Probabilistic seismic hazard assessment (PSHA) is conducted based on characteristic earthquake modelling for the fault segments capable of producing large earthquakes and smoothed seismicity modelling for the background smaller magnitude earthquake activity. The time-independent and time-dependent seismic hazard results in terms of spatial distributions of three ground-shaking intensity measures (peak ground acceleration, PGA, and 0.2 s and 1.0 s spectral accelerations (SA) on rock having 10% and 2% probabilities of exceedance in 50 years) as well as the corresponding hazard curves for selected cities are shown and compared with previous studies.https://www.mdpi.com/2076-3263/9/12/489probabilistic seismic hazard assessmentrenewal and poisson modelsmarmara regionturkeynorth anatolian fault zone |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Karin Şeşetyan Mine Betül Demircioğlu Tümsa Aybige Akinci |
spellingShingle |
Karin Şeşetyan Mine Betül Demircioğlu Tümsa Aybige Akinci Evaluation of The Seismic Hazard in The Marmara Region (Turkey) Based on Updated Databases Geosciences probabilistic seismic hazard assessment renewal and poisson models marmara region turkey north anatolian fault zone |
author_facet |
Karin Şeşetyan Mine Betül Demircioğlu Tümsa Aybige Akinci |
author_sort |
Karin Şeşetyan |
title |
Evaluation of The Seismic Hazard in The Marmara Region (Turkey) Based on Updated Databases |
title_short |
Evaluation of The Seismic Hazard in The Marmara Region (Turkey) Based on Updated Databases |
title_full |
Evaluation of The Seismic Hazard in The Marmara Region (Turkey) Based on Updated Databases |
title_fullStr |
Evaluation of The Seismic Hazard in The Marmara Region (Turkey) Based on Updated Databases |
title_full_unstemmed |
Evaluation of The Seismic Hazard in The Marmara Region (Turkey) Based on Updated Databases |
title_sort |
evaluation of the seismic hazard in the marmara region (turkey) based on updated databases |
publisher |
MDPI AG |
series |
Geosciences |
issn |
2076-3263 |
publishDate |
2019-11-01 |
description |
The increase in the wealth of information on the seismotectonic structure of the Marmara region after two devastating earthquakes (<b>M</b>7.6 Izmit and <b>M</b>7.2 Duzce events) in the year 1999 opened the way for the reassessment of the probabilistic seismic hazard in the light of new datasets. In this connection, the most recent findings and outputs of different national and international projects concerning seismicity and fault characterization in terms of geometric and kinematic properties are exploited in the present study to build an updated seismic hazard model. A revised fault segmentation model, alternative earthquake rupture models under a Poisson and renewal assumptions, as well as recently derived global and regional ground motion prediction equations (GMPEs) are put together in the present model to assess the seismic hazard in the region. Probabilistic seismic hazard assessment (PSHA) is conducted based on characteristic earthquake modelling for the fault segments capable of producing large earthquakes and smoothed seismicity modelling for the background smaller magnitude earthquake activity. The time-independent and time-dependent seismic hazard results in terms of spatial distributions of three ground-shaking intensity measures (peak ground acceleration, PGA, and 0.2 s and 1.0 s spectral accelerations (SA) on rock having 10% and 2% probabilities of exceedance in 50 years) as well as the corresponding hazard curves for selected cities are shown and compared with previous studies. |
topic |
probabilistic seismic hazard assessment renewal and poisson models marmara region turkey north anatolian fault zone |
url |
https://www.mdpi.com/2076-3263/9/12/489 |
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