{"id":129,"date":"2024-02-22T18:05:33","date_gmt":"2024-02-22T18:05:33","guid":{"rendered":"http:\/\/193.194.89.193\/wp_lge\/?page_id=129"},"modified":"2024-02-22T18:22:52","modified_gmt":"2024-02-22T18:22:52","slug":"communications-2010","status":"publish","type":"page","link":"https:\/\/lge.usthb.dz\/index.php\/communications-2010\/","title":{"rendered":"Communications 2010"},"content":{"rendered":"\n<ul class=\"wp-block-list\">\n<li>NAAK M., 2010. La fracturation t\u00e9thysienne au Lias dans le Djurdjura, mise en place d\u2019une marge continentale passive et la premi\u00e8re diff\u00e9renciation structurale et pal\u00e9og\u00e9ographique au sein de cette plateforme. Journ\u00e9es Scientifiques de la FSTGAT\/USTHB.<\/li>\n<\/ul>\n\n\n\n<h1 class=\"wp-block-heading\"><\/h1>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-129","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/lge.usthb.dz\/index.php\/wp-json\/wp\/v2\/pages\/129","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/lge.usthb.dz\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/lge.usthb.dz\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/lge.usthb.dz\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/lge.usthb.dz\/index.php\/wp-json\/wp\/v2\/comments?post=129"}],"version-history":[{"count":3,"href":"https:\/\/lge.usthb.dz\/index.php\/wp-json\/wp\/v2\/pages\/129\/revisions"}],"predecessor-version":[{"id":145,"href":"https:\/\/lge.usthb.dz\/index.php\/wp-json\/wp\/v2\/pages\/129\/revisions\/145"}],"wp:attachment":[{"href":"https:\/\/lge.usthb.dz\/index.php\/wp-json\/wp\/v2\/media?parent=129"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}