Earthquake Swarms, Slow Slip and Fault Interactions at the Western‐End of the Hellenic Subduction System Precede the Mw 6.9 Zakynthos Earthquake, Greece

Abstract The month‐to‐year‐long deformation of the Earth's crust where active subduction zones terminate is poorly explored. Here we report on a multidisciplinary data set that captures the synergy of slow‐slip events, earthquake swarms and fault interactions during the ∼5 years leading up to the 20...

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Hlavní autoři:	Vasiliki Mouslopoulou, Gian Maria Bocchini, Simone Cesca, Vasso Saltogianni, Jonathan Bedford, Gesa Petersen, Michael Gianniou, Onno Oncken
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2020-12-01
Edice:	Geochemistry, Geophysics, Geosystems
Témata:	Hellenic subduction microseismicity plate‐interface slow slip events upper‐plate Zakynthos Earthquake
On-line přístup:	https://doi.org/10.1029/2020GC009243
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