project ASPIDA “Infrastructure Upgrade for Seismic Protection of the Country and 361 Strengthen Service Excellence through Action”, project MIS-448326, implemented under 362 the Action “Development Propo
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In this paper we present new geological and seismological data on the orientation of crustal extension in central Crete (SE Heraklion basin) following the occurrence of two shallow seismic sequences: a) the May 2005 Assimi M=4.1 earthquake sequence and b) the 2013 Houdetsi-Tefeli sequence (3.2≤Mw≤3.6). Emphasis is given to the results of the geological field work, stress analysis, source inversion, aftershock relocations and mapping of earthquake-induced environmental effects. For the first time we find seismological evidence for N-S strike-slip motions along shallow fault planes in central Crete (Amourgeles fault). Our results indicate that while crustal extension dominates there is a combination of active fault kinematics, ranging from normal faulting along the northern edge of Messara basin (south-dipping Plakiotissa fault) to strike-slip faulting inside the SE part Heraklion basin (Houdetsi-Tefeli). The combination of active fault motions accommodates a NW-SE extension of the upper crust.
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Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Vol 51 (2017): Bulletin of the Geological Society of Greece, Vol. LI-51,; 52-75
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Bulletin of the Geological Society of Greece; Vol 51 (2017): Bulletin of the Geological Society of Greece, Vol. LI-51,; 52-75
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Copyright (c) 2017 Athanassios Ganas, Charalambos Fassoulas, Alexandra Moshou, George Bozionelos, George Papathanassiou, Christina Tsimi, Sotirios Valkaniotis
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