1,721,115 research outputs found
Fault Interaction and the Evolution of Seismicity: the Case Study of the Central Apennine Fault System (CAFS)
This thesis presents an integrated study of the Central Apennine Fault System (CAFS),
focusing on the dynamics of fault interactions and the role of Coulomb Stress Transfer
(CST) in shaping seismicity. The CAFS, a seismically active region in central Italy,
has witnessed numerous destructive earthquakes recorded in extensive national
seismic catalogs, making it an ideal subject for investigating the mechanisms
underlying seismic events and their respective seismic cycles. In addition to the CAFS,
the thesis incorporates findings from a field-based analysis of the Mw 6.4 Petrinja
earthquake in Croatia. Although geographically distinct from the CAFS, this study
contributes valuable insights into the processes of coseismic faulting and fault
interaction in a strike-slip environment, enhancing our understanding of fault
dynamics across different tectonic settings.
The proposed study spans a variety of tectonic regimes but aims to converge on a
detailed examination of fault interaction and the related seismic activity. The primary
focus is, therefore, on understanding how the CST influences the activation and
interaction of faults within this intricate system in central Italy. A significant aspect of
this research involves the analysis of both historical and instrumental seismic events
within the CAFS, spanning from the year 1200 AD to the present day. Employing
advanced modeling techniques, including innovative three-dimensional elliptical
models, the study provides new insights into the role of CST in fault activity. The
research demonstrates that CST plays a pivotal role in either promoting or inhibiting
seismic events, highlighting the importance of this mechanism in understanding the
seismic cycle of the region.
This thesis aims to advance the knowledge of Earthquake Geology by providing a
comprehensive understanding of the seismic mechanisms within the CAFS and in
regions that are geographically and geologically distinct (e.g., Petrinja, Croatia). The
findings of this research might have significant implicationsfor seismic hazard
assessment and risk management, contributing to the development of targeted
seismic risk mitigation strategies and enhancing efforts in earthquake preparedness
and response in seismically active regions
Fault Interaction and the Evolution of Seismicity: the Case Study of the Central Apennine Fault System (CAFS)
This thesis presents an integrated study of the Central Apennine Fault System (CAFS),
focusing on the dynamics of fault interactions and the role of Coulomb Stress Transfer
(CST) in shaping seismicity. The CAFS, a seismically active region in central Italy,
has witnessed numerous destructive earthquakes recorded in extensive national
seismic catalogs, making it an ideal subject for investigating the mechanisms
underlying seismic events and their respective seismic cycles. In addition to the CAFS,
the thesis incorporates findings from a field-based analysis of the Mw 6.4 Petrinja
earthquake in Croatia. Although geographically distinct from the CAFS, this study
contributes valuable insights into the processes of coseismic faulting and fault
interaction in a strike-slip environment, enhancing our understanding of fault
dynamics across different tectonic settings.
The proposed study spans a variety of tectonic regimes but aims to converge on a
detailed examination of fault interaction and the related seismic activity. The primary
focus is, therefore, on understanding how the CST influences the activation and
interaction of faults within this intricate system in central Italy. A significant aspect of
this research involves the analysis of both historical and instrumental seismic events
within the CAFS, spanning from the year 1200 AD to the present day. Employing
advanced modeling techniques, including innovative three-dimensional elliptical
models, the study provides new insights into the role of CST in fault activity. The
research demonstrates that CST plays a pivotal role in either promoting or inhibiting
seismic events, highlighting the importance of this mechanism in understanding the
seismic cycle of the region.
This thesis aims to advance the knowledge of Earthquake Geology by providing a
comprehensive understanding of the seismic mechanisms within the CAFS and in
regions that are geographically and geologically distinct (e.g., Petrinja, Croatia). The
findings of this research might have significant implicationsfor seismic hazard
assessment and risk management, contributing to the development of targeted
seismic risk mitigation strategies and enhancing efforts in earthquake preparedness
and response in seismically active regions
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