{"id":1154,"date":"2022-09-10T13:16:00","date_gmt":"2022-09-10T13:16:00","guid":{"rendered":"http:\/\/adriendamon-geoconsulting.pro\/?p=1154"},"modified":"2025-09-24T12:52:01","modified_gmt":"2025-09-24T12:52:01","slug":"pata-workshop-paleoseismology-active-tectonics-and-archeoseismology","status":"publish","type":"post","link":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/2022\/09\/10\/pata-workshop-paleoseismology-active-tectonics-and-archeoseismology\/","title":{"rendered":"PATA workshop – paleoseismology, active tectonics and archeoseismology"},"content":{"rendered":"\n
\n
\n

I am glad to have participated in this workshop (https:\/\/patadays-2022.sciencesconf.org\/<\/a>), it has been an interesting event with much discussion and an interesting fieldtrip to study active tectonics markers in the franco-italian Alps and southeastern France.<\/p>\n<\/div>\n\n\n\n

\n
\"\"<\/figure>\n\n\n

Featured image: scarp of a fault of recent (quaternary) activity near the Lombarde pass studied during the fieldtrip.<\/p>\n<\/div>\n<\/div>\n<\/div>\n\n\n\n

\n
\n
\"\"
Presentation of my work on the effects of glacial isostasy in the Paris Basin on fault stability in response to glacial cycles (past and future).<\/figcaption><\/figure>\n<\/div>\n\n\n\n
\n
\"\"
Trench crossing the “La Rouvi\u00e8re” fault in southeastern France, allowing the study of its recent activity, with the aim to identify eventual holocene-quaternary movements. More informations in Ritz et al. (2020): Surface rupture and shallow fault reactivation during the 2019 Mw 4.9 Le Teil earthquake, France<\/a> and Ritz et al. (2022): The 2019 Le Teil surface-rupturing earthquake along the La Rouvi\u00e8re Fault within the C\u00e9vennes fault system (France): What does paleoseismology reveal?<\/a><\/figcaption><\/figure>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"

I am glad to have participated in this workshop (https:\/\/patadays-2022.sciencesconf.org\/), it has been an interesting event with much discussion and an interesting fieldtrip to study active tectonics markers in the franco-italian Alps and southeastern France. Featured image: scarp of a fault of recent (quaternary) activity near the Lombarde pass studied during the fieldtrip.<\/p>\n","protected":false},"author":1,"featured_media":1155,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-1154","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/posts\/1154","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/comments?post=1154"}],"version-history":[{"count":8,"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/posts\/1154\/revisions"}],"predecessor-version":[{"id":1212,"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/posts\/1154\/revisions\/1212"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/media\/1155"}],"wp:attachment":[{"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/media?parent=1154"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/categories?post=1154"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/adriendamon-geoconsulting.pro\/index.php\/wp-json\/wp\/v2\/tags?post=1154"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}