Micro-seismicity, seismic-wave velocity model and earthquake clustering in the Akarnanian region (western Greece)
Authors: Lefils Valentine , Rigo Alexis , Sokos Efthimios 
Published: March 2021

&lt;p&gt;Characterized for the first time in 2013, the Island Akarnanian Block (IAB) is a micro-plate located in the western Greece. This micro-plate accommodates the deformation in between larger scale tectonic structures as the Gulf of Corinth (South-East), the Hellenic subduction (South) and the Apulian Collison (West).&lt;/p&gt;&lt;p&gt;&lt;span&gt;W&lt;/span&gt;&lt;span&gt;e &lt;/span&gt;&lt;span&gt;start&lt;/span&gt;&lt;span&gt;ed a micro-seismic &lt;/span&gt;&lt;span&gt;survey&lt;/span&gt;&lt;span&gt; (MADAM) at the end of 2015 with a dense seismological network &lt;/span&gt;&lt;span&gt;over the area, between the Gulf of Patras and the Gulf of Amvrakikos. &lt;/span&gt;&lt;span&gt;In order t&lt;/span&gt;&lt;span&gt;o obtain precise locations of the recorded events, we better constrained the local velocity model. In fact, &lt;/span&gt;&lt;span&gt;s&lt;/span&gt;&lt;span&gt;everal velocity models &lt;/span&gt;&lt;span&gt;(local or regional) &lt;/span&gt;&lt;span&gt;have been proposed for this area. &lt;/span&gt;&lt;span&gt;H&lt;/span&gt;&lt;span&gt;owever,&lt;/span&gt;&lt;span&gt; the velocity model generally used by the scientific community remains the Hasslinger 98 velocity model. This model, nevertheless, raises some questions about its physical meaning, mainly due to a low velocity layer bet&lt;/span&gt;&lt;span&gt;w&lt;/span&gt;&lt;span&gt;ee&lt;/span&gt;&lt;span&gt;n &lt;/span&gt;&lt;span&gt;4 and 7 km-depth. &lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;Thanks to our seismological network and permanent networks of the Corinth Rift Laboratory and the Hellenic Unified Seismic Network, w&lt;/span&gt;&lt;span&gt;e colle&lt;/span&gt;&lt;span&gt;c&lt;/span&gt;&lt;span&gt;ted and anal&lt;/span&gt;&lt;span&gt;y&lt;/span&gt;&lt;span&gt;s&lt;/span&gt;&lt;span&gt;ed&lt;/span&gt;&lt;span&gt; a huge quantity of data &lt;/span&gt;&lt;span&gt;a&lt;/span&gt;&lt;span&gt;c&lt;/span&gt;&lt;span&gt;quired &lt;/span&gt;&lt;span&gt;between &lt;/span&gt;&lt;span&gt;O&lt;/span&gt;&lt;span&gt;ctober 2015 and &lt;/span&gt;&lt;span&gt;D&lt;/span&gt;&lt;span&gt;ecember 2017. &lt;/span&gt;&lt;span&gt;Those analyses of &lt;/span&gt;&lt;span&gt;more than &lt;/span&gt;&lt;span&gt;10,000&lt;/span&gt;&lt;span&gt; events allowed us to &lt;/span&gt;&lt;span&gt;develop &lt;/span&gt;&lt;span&gt;a new &lt;/span&gt;&lt;span&gt;and robust &lt;/span&gt;&lt;span&gt;local velocity model, &lt;/span&gt;&lt;span&gt;wh&lt;/span&gt;&lt;span&gt;ich&lt;/span&gt;&lt;span&gt; is consi&lt;/span&gt;&lt;span&gt;s&lt;/span&gt;&lt;span&gt;tent with the seismic data and &lt;/span&gt;&lt;span&gt;the &lt;/span&gt;&lt;span&gt;geophysical obse&lt;/span&gt;&lt;span&gt;r&lt;/span&gt;&lt;span&gt;vations&lt;/span&gt;&lt;span&gt;.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;The observed seismic activity is characterized by the presence of numerous clusters. The clusters are analysed in detail by relative relocations in order to appraise their physical processes and their possible implications in the fault activity to finally have a better understanding of the deformation mode(s) of the IAB micro-plate.&lt;/p&gt;