<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</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><author><style face="normal" font="default" size="100%">Hatzfeld, D.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">&lt;span style=&quot;font-family: Arial, sans-serif;&quot;&gt;&lt;span style=&quot;font-size: 13.3333px;&quot;&gt;&lt;strong&gt;Elastic-Anelastic Properties of the Aegean Lithosphere-Asthenosphere Inferred from Long Period Rayleigh Waves&lt;/strong&gt;&lt;/span&gt;&lt;/span&gt;</style></title><secondary-title><style face="normal" font="default" size="100%">The Lithosphere: Geochemistry, Geology and Geophysics</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.novapublishers.org/catalog/product_info.php?products_id=7638</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">Nova Science Pub Inc</style></publisher><pages><style face="normal" font="default" size="100%">267-294</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The highest deformation rate along the Africa/Eurasia convergence zone is well&lt;br&gt;documented in the Aegean area, being &amp;gt;4 cm/yr. However, it is still under question whether&lt;br&gt;continental deformation is distributed along major faults which extend through the whole&lt;br&gt;lithosphere or over large areas. Furthermore, our knowledge concerning the implication of&lt;br&gt;lithosphere-asthenosphere coupling in lithospheric plates driving forces is poor. These&lt;br&gt;questions can not easily be answered as most of the available information is mainly located at&lt;br&gt;or close to the surface (geodesy, tectonics, seismicity). The high rates and type of surface&lt;br&gt;continental deformation within the Aegean constitute this region particularly interesting in this&lt;br&gt;perspective.&lt;br&gt;This work is towards contributing to the better knowledge of the physical properties of&lt;br&gt;the Aegean lithosphere by introducing experimental elastic and anelastic parameters inferred&lt;br&gt;from long period Rayleigh wave. For this scope path-average phase velocities and attenuation&lt;br&gt;coefficients of fundamental Rayleigh wave crossing the Aegean were extracted over the&lt;br&gt;period range 10-100 s. The wavetrains were recorded at the temporary broadband stations&lt;br&gt;installed some years ago in the Aegean region within the framework of a large scale&lt;br&gt;experiment (SEISFAULTGREECE project).&lt;/p&gt;</style></abstract></record></records></xml>