{"id":287,"date":"2021-01-13T11:24:12","date_gmt":"2021-01-13T11:24:12","guid":{"rendered":"http:\/\/lptms.u-psud.fr\/alberto_rosso\/?page_id=287"},"modified":"2021-01-13T16:37:54","modified_gmt":"2021-01-13T16:37:54","slug":"80-prime","status":"publish","type":"page","link":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/80-prime\/","title":{"rendered":"80 PRIME"},"content":{"rendered":"<p><strong>Temporal spatial correlations in earthquakes dynamics: physical modelling and data anlysis<\/strong><\/p>\n<p><strong>R\u00e9sum\u00e9 du projet<\/strong><\/p>\n<p>One of the most distinctive and poorly understood feature of earthquakes is the significant increase of the<\/p>\n<p>seismic rate observed after large events. Well established empirical laws of aftershocks occurrence<\/p>\n<p>demand for a physical explanation. Foreshocks are also observed before a large event but their statistical<\/p>\n<p>fingerprints, potentially important for human security, are much more elusive. In this project, using the<\/p>\n<p>methods developed in the Statistical Physics we will design a model of the fault able to reproduce complex<\/p>\n<p>spatio-temporal patterns with foreshocks, mainshocks and aftershocks. Using Machine Learning we will<\/p>\n<p>understand the statistical properties of the short sequence of foreshocks. First, using our synthetic<\/p>\n<p>sequences, we determine how much information is needed to predict the following events. Then we will<\/p>\n<p>use actual data: on one side to calibrate the model on the real fault activity, on the other side to predict<\/p>\n<p>how dangerous is a real sequence of foreshocks.<\/p>\n<p>&nbsp;<\/p>\n<p><strong>Team:<\/strong><\/p>\n<ul>\n<li>A. Rosso &amp; V. M. Schimmenti (LPTMS)<\/li>\n<li>F. Landes &amp; M. Schoenauer (LISN)<\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>Temporal spatial correlations in earthquakes dynamics: physical modelling and data anlysis R\u00e9sum\u00e9 du projet One of the most distinctive and poorly understood feature of earthquakes is the significant increase of the seismic rate observed after large events. Well established empirical &hellip; <a href=\"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/80-prime\/\">Continuer la lecture <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":4,"featured_media":330,"parent":0,"menu_order":4,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-287","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/pages\/287","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/comments?post=287"}],"version-history":[{"count":5,"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/pages\/287\/revisions"}],"predecessor-version":[{"id":333,"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/pages\/287\/revisions\/333"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/media\/330"}],"wp:attachment":[{"href":"http:\/\/www.lptms.universite-paris-saclay.fr\/alberto_rosso\/wp-json\/wp\/v2\/media?parent=287"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}