The 2020 Perachora peninsula earthquake sequence (Εast Corinth Rift, Greece): spatiotemporal evolution and implications for the triggering mechanism

Michas, Georgios; Kapetanidis, Vasilis; Spingos, Ioannis; Kaviris, George; Vallianatos, Filippos

doi:10.1007/s11600-022-00864-x

Artykuł - szczegóły

Tytuł artykułu

The 2020 Perachora peninsula earthquake sequence (Εast Corinth Rift, Greece): spatiotemporal evolution and implications for the triggering mechanism

Autorzy

Michas Georgios , Kapetanidis Vasilis , Spingos Ioannis , Kaviris George , Vallianatos Filippos

Wybrane pełne teksty z tego czasopisma

https://www.springer.com/journal/11600

Identyfikatory

DOI

10.1007/s11600-022-00864-x

Warianty tytułu

Języki publikacji

Abstrakty

In this work, we study the January 1, 2020 – June 8, 2021, earthquake activity in the East Corinth Rift (central Greece), one of the most seismically active areas in Europe. During this period an intense earthquake sequence occurred in the Perachora peninsula, presenting the characteristics of swarm activity. We present a relocated earthquake catalogue for the area, derived with the double-difference algorithm, and study the spatiotemporal evolution of the 2020 Perachora peninsula earthquake sequence and the possible triggering mechanisms. The Perachora sequence presents distinct characteristics of earthquake migration along a N 103º E direction, as indicated by the Principal Component Analysis, from the east toward northwest and then west, with successive deepening of the events. This migration pattern is compatible with a pore-fluid pressure triggering front of hydraulic diffusivity of D =2.8 m2 /s and an average velocity of 0.22 km/day. In addition, the sequence presents sub-diffusion, with a diffusion exponent of 0.89±0.06. The analysis, overall, indicates that the Perachora sequence was triggered at shallow depths by fluid overpressures, possibly generated by down-going fuxes of meteoric fluids, and then driven by pore-fluid pressure diffusion along the activated structures.

Słowa kluczowe

Corinth Rift earthquake migration aseismic triggering subdiffusion Perachora swarm pore-fluid pressure diffusion

Szczelina Koryncka migracja trzęsienia ziemi wyzwalanie asejsmiczne subdyfuzja

Wydawca

Instytut Geofizyki PAN
Springer

Czasopismo

Acta Geophysica

Rocznik

2022

Tom

Vol. 70, no 6

Strony

2581--2601

Opis fizyczny

Bibliogr. 90 poz.

Twórcy

autor

Michas Georgios

gemichas@geol.uoa.gr

Section of Geophysics–Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Athens, Greece

https://orcid.org/0000-0002-0284-3867

autor

Kapetanidis Vasilis

Section of Geophysics–Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Athens, Greece

autor

Spingos Ioannis

Section of Geophysics–Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Athens, Greece

autor

Kaviris George

Section of Geophysics–Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Athens, Greece

autor

Vallianatos Filippos

Section of Geophysics–Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Athens, Greece
Institute of Physics of Earth’s Interior and Geohazards, UNESCO Chair On Solid Earth Physics and Geohazards Risk Reduction, Hellenic Mediterranean University Research Center, Crete, Greece

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Uwagi

Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).

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Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-0aee87dc-8969-41c3-a5ee-0b8c63cf8a8e