<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Kassaras, I.</style></author><author><style face="normal" font="default" size="100%">F. Louis</style></author><author><style face="normal" font="default" size="100%">Makropoulos, K.</style></author><author><style face="normal" font="default" size="100%">A. Magganas</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Shear velocity and intrinsic attenuation variation within the Aegean Lithosphere deduced from surface waves</style></title><secondary-title><style face="normal" font="default" size="100%">31st General Assembly of the European Seismological Commission</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://drive.google.com/file/d/1oo-2RpjhRR2lZ_P1c0KR26LBCcpYxREv/view</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%"> European Seismological Commission</style></publisher><pub-location><style face="normal" font="default" size="100%">Crete (Greece)</style></pub-location><pages><style face="normal" font="default" size="100%">206-213</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;This paper presents a new shear velocity and attenuation model for the lower crust and litho-&lt;br&gt;sphere of the Aegean region, obtained by inversion of broadband surface-wave phase veloci-&lt;br&gt;ties and attenuation coefficients. We have two main motivations for conducting this study.&amp;nbsp;First, knowledge of the regional structure of the Aegean lithosphere is fundamental for understanding the tectonic framework and mantle dynamics, posing constraints on possible models&amp;nbsp;of deformation and evolution. Second, the exponential dependence of Q with temperature&amp;nbsp;implies that attenuation tomography could explain better hot regions (high attenuation) than&amp;nbsp;elastic tomography. Furthermore, elastic velocity is highly influenced by the constitution of the&amp;nbsp;medium. In case of strong lateral Q variations, elastic parameters also vary. Hence, it is important to combine results of elastic and anelastic tomography. Apparently, the high rates of&amp;nbsp;deformation in the Aegean constitute this region particularly interesting in this perspective.&lt;/p&gt;</style></abstract></record></records></xml>