Long-Term Recurrence Pattern and Stress Transfer along the Kefalonia Transform Fault Zone (KTFZ), Greece: Implications in Seismic Hazard Evaluation

An effort is exerted to investigate the recurrence pattern of large earthquakes (<i>M<sub>w</sub></i> ≥ 6.0) in the Kefalonia Transform Fault Zone (KTFZ), Greece, by considering the incorporation of the 74-year (1948–2022) evolving stress field. Four earthquake occurrence mod...

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Main Authors: Christos Kourouklas, Eleftheria Papadimitriou, Vasileios Karakostas
Format: Article
Language:English
Published: MDPI AG 2023-09-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/13/10/295
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author Christos Kourouklas
Eleftheria Papadimitriou
Vasileios Karakostas
author_facet Christos Kourouklas
Eleftheria Papadimitriou
Vasileios Karakostas
author_sort Christos Kourouklas
collection DOAJ
description An effort is exerted to investigate the recurrence pattern of large earthquakes (<i>M<sub>w</sub></i> ≥ 6.0) in the Kefalonia Transform Fault Zone (KTFZ), Greece, by considering the incorporation of the 74-year (1948–2022) evolving stress field. Four earthquake occurrence models—the Poisson, Poisson with the incorporation of the static stress changes (Poisson + Δ<i>CFF</i>), Brownian passage time (BPT) and Brownian passage time with the incorporation of the static stress changes (BPT + Δ<i>CFF</i>)—have been applied to estimate the occurrence probabilities of nearly characteristic earthquakes for the seven fault segments of the study area. The mean recurrence time, <i>T<sub>r</sub></i>, is estimated using the physics-based seismic moment rate conservation method. The results show large variability depending upon fault parameters. Incorporating the state of stress into <i>T<sub>r</sub></i> results in both advanced and delayed recurrence patterns. The occurrence probability estimates for the next 10, 20 and 30 years indicate that the fault segment most likely to be ruptured is the Paliki North fault segment in all models. Overall, the occurrence probabilities, combined with the state of stress along the fault segments, emphasize the high seismic moment rate of the study area. The application of time-dependent models (BPT, BPT + Δ<i>CFF</i>) resulted in significant increases or decreases in the associated seismic hazard.
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spelling doaj.art-cd8d1a9a5170422187954eab3c285bd22023-11-19T16:36:15ZengMDPI AGGeosciences2076-32632023-09-01131029510.3390/geosciences13100295Long-Term Recurrence Pattern and Stress Transfer along the Kefalonia Transform Fault Zone (KTFZ), Greece: Implications in Seismic Hazard EvaluationChristos Kourouklas0Eleftheria Papadimitriou1Vasileios Karakostas2Geophysics Department, School of Geology, Aristotle University of Thessaloniki, 54124 Thessaloniki, GreeceGeophysics Department, School of Geology, Aristotle University of Thessaloniki, 54124 Thessaloniki, GreeceGeophysics Department, School of Geology, Aristotle University of Thessaloniki, 54124 Thessaloniki, GreeceAn effort is exerted to investigate the recurrence pattern of large earthquakes (<i>M<sub>w</sub></i> ≥ 6.0) in the Kefalonia Transform Fault Zone (KTFZ), Greece, by considering the incorporation of the 74-year (1948–2022) evolving stress field. Four earthquake occurrence models—the Poisson, Poisson with the incorporation of the static stress changes (Poisson + Δ<i>CFF</i>), Brownian passage time (BPT) and Brownian passage time with the incorporation of the static stress changes (BPT + Δ<i>CFF</i>)—have been applied to estimate the occurrence probabilities of nearly characteristic earthquakes for the seven fault segments of the study area. The mean recurrence time, <i>T<sub>r</sub></i>, is estimated using the physics-based seismic moment rate conservation method. The results show large variability depending upon fault parameters. Incorporating the state of stress into <i>T<sub>r</sub></i> results in both advanced and delayed recurrence patterns. The occurrence probability estimates for the next 10, 20 and 30 years indicate that the fault segment most likely to be ruptured is the Paliki North fault segment in all models. Overall, the occurrence probabilities, combined with the state of stress along the fault segments, emphasize the high seismic moment rate of the study area. The application of time-dependent models (BPT, BPT + Δ<i>CFF</i>) resulted in significant increases or decreases in the associated seismic hazard.https://www.mdpi.com/2076-3263/13/10/295large earthquake recurrence timestatic stress transferstress triggeringstatistical analysisKefalonia Transform Fault ZoneGreece
spellingShingle Christos Kourouklas
Eleftheria Papadimitriou
Vasileios Karakostas
Long-Term Recurrence Pattern and Stress Transfer along the Kefalonia Transform Fault Zone (KTFZ), Greece: Implications in Seismic Hazard Evaluation
Geosciences
large earthquake recurrence time
static stress transfer
stress triggering
statistical analysis
Kefalonia Transform Fault Zone
Greece
title Long-Term Recurrence Pattern and Stress Transfer along the Kefalonia Transform Fault Zone (KTFZ), Greece: Implications in Seismic Hazard Evaluation
title_full Long-Term Recurrence Pattern and Stress Transfer along the Kefalonia Transform Fault Zone (KTFZ), Greece: Implications in Seismic Hazard Evaluation
title_fullStr Long-Term Recurrence Pattern and Stress Transfer along the Kefalonia Transform Fault Zone (KTFZ), Greece: Implications in Seismic Hazard Evaluation
title_full_unstemmed Long-Term Recurrence Pattern and Stress Transfer along the Kefalonia Transform Fault Zone (KTFZ), Greece: Implications in Seismic Hazard Evaluation
title_short Long-Term Recurrence Pattern and Stress Transfer along the Kefalonia Transform Fault Zone (KTFZ), Greece: Implications in Seismic Hazard Evaluation
title_sort long term recurrence pattern and stress transfer along the kefalonia transform fault zone ktfz greece implications in seismic hazard evaluation
topic large earthquake recurrence time
static stress transfer
stress triggering
statistical analysis
Kefalonia Transform Fault Zone
Greece
url https://www.mdpi.com/2076-3263/13/10/295
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