{"id":68,"date":"2020-06-04T11:28:51","date_gmt":"2020-06-04T08:28:51","guid":{"rendered":"http:\/\/blogs.upatras.gr\/zroumelioti\/?page_id=68"},"modified":"2024-12-15T18:35:34","modified_gmt":"2024-12-15T15:35:34","slug":"research-interests","status":"publish","type":"page","link":"https:\/\/blogs.upatras.gr\/zroumelioti\/research-interests\/","title":{"rendered":""},"content":{"rendered":"<div id=\"main2\">\n<h2>Main Research Topics<\/h2>\n<ul>\n<li>Seismic Hazard<\/li>\n<li>Simulation of strong ground motion using both deterministic (Empirical Green&#8217;s Functions) and stochastic approaches with emphasis on the incorporation of the finite-source and directivity effects<\/li>\n<li>Kinematic modeling of earthquake sources; Determination of the spatio-temporal characteristics of earthquake rupture by i) inversion of full waveforms at regional and\/or teleseismic distances, geodetic data, strong ground motion records and surface offset data and ii) inversion of relative source time functions<\/li>\n<li>Variability of strong ground motion due to source and site effects<\/li>\n<li>Near-fault effects on strong ground motion<\/li>\n<li>Near real-time applications for the computation of earthquake source parameters (fast moment tensors) and shake maps for earthquakes in areas covered by sparse networks<\/li>\n<li>Moment tensor determination<\/li>\n<li>Study of non-linear site response during earthquakes<\/li>\n<li>Seismicity studies (relocation, determination of source parameters, seismotectonic implications)<\/li>\n<li>Shallow Geophysics for Site Characterization<\/li>\n<li>Geophysics for Archaeology<\/li>\n<\/ul>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Main Research Topics Seismic Hazard Simulation of strong ground motion using both deterministic (Empirical Green&#8217;s Functions) and stochastic approaches with emphasis on the incorporation of the finite-source and directivity effects Kinematic modeling of earthquake sources; Determination of the spatio-temporal characteristics of earthquake rupture by i) inversion of full waveforms at regional and\/or teleseismic distances, geodetic data, strong ground motion records and surface offset data and ii) inversion of relative source time functions Variability of strong ground motion due to source and site effects Near-fault effects on strong ground motion Near real-time applications for the computation of earthquake source parameters (fast moment tensors) and shake maps for earthquakes in areas covered &#8230;<\/p>\n","protected":false},"author":76,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-templates\/full-width.php","meta":{"footnotes":""},"class_list":["post-68","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/blogs.upatras.gr\/zroumelioti\/wp-json\/wp\/v2\/pages\/68","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.upatras.gr\/zroumelioti\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/blogs.upatras.gr\/zroumelioti\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.upatras.gr\/zroumelioti\/wp-json\/wp\/v2\/users\/76"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.upatras.gr\/zroumelioti\/wp-json\/wp\/v2\/comments?post=68"}],"version-history":[{"count":7,"href":"https:\/\/blogs.upatras.gr\/zroumelioti\/wp-json\/wp\/v2\/pages\/68\/revisions"}],"predecessor-version":[{"id":178,"href":"https:\/\/blogs.upatras.gr\/zroumelioti\/wp-json\/wp\/v2\/pages\/68\/revisions\/178"}],"wp:attachment":[{"href":"https:\/\/blogs.upatras.gr\/zroumelioti\/wp-json\/wp\/v2\/media?parent=68"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}