Kkallas, Ch. http://orcid.org/0000-0002-5608-9214
Papazachos, C. B.
Boore, D.
Ventouzi, Ch.
Margaris, B. N.
Article History
Received: 5 July 2017
Accepted: 28 February 2018
First Online: 5 March 2018
Data and resources
: The intermediate-depth earthquake data used in Fig. InternalRef removedare available atExternalRef removed(last accessed December 2017). The EXSIM_DMB code used for the simulations is available atExternalRef removed(last accessed December 2017). Macroseismic intensities of historical events were collected from the database of macroseismic information for the Aegean area (Papazachos et al.CitationRef removed), available upon request, as well as from the online bulletin of the International Seismological Center (ExternalRef removed) and the online archives of the Bureau Central Sismologique Français (ExternalRef removed). Broadband velocity-sensor data were collected from permanent Greek seismological networks, operated by the Hellenic Unified Seismological Network (HUSN), available to the public upon request from individual HUSN members. Strong motion data employed in this work were collected from the permanent networks operated by the Institute of Engineering Seismology and Earthquake Engineering (ITSAK) and the National Observatory of Athens, which are also available upon request. Several plots were made using the Generic Mapping Tools version 4 (Wessel and SmithCitationRef removed;ExternalRef removed, last accessed December 2017).