{"id":8336,"date":"2021-02-28T14:34:21","date_gmt":"2021-02-28T13:34:21","guid":{"rendered":"http:\/\/synthese.univ-annaba.dz\/?p=8336"},"modified":"2021-02-28T14:35:19","modified_gmt":"2021-02-28T13:35:19","slug":"etude-sedimentologique-de-la-serie-neritique-carbonatee-cenomano-albienne-du-groupe-oriental-constantinois-cas-djebel-grar-n-e-algerien","status":"publish","type":"post","link":"https:\/\/synthese.univ-annaba.dz\/?p=8336","title":{"rendered":"Etude s\u00e9dimentologique de la s\u00e9rie n\u00e9ritique carbonat\u00e9e C\u00e9nomano-Albienne du groupe oriental Constantinois \u2013 Cas : Djebel Grar (N. E. Alg\u00e9rien)"},"content":{"rendered":"<div><strong>Num\u00e9ro de la revue<\/strong>: Volume 26 , Num\u00e9ro 1<\/div>\n<p><strong>Manal Bouchama<sup>*<\/sup>&amp; Fella Assassi<\/strong><\/p>\n<p>D\u00e9partement de G\u00e9ologie, Universit\u00e9 Badji-Mokhtar, BP 12, Annaba 23000, Alg\u00e9rie.<\/p>\n<p>&nbsp;<\/p>\n<div>\n<p style=\"text-align: right;\"><a href=\"http:\/\/synthese.univ-annaba.dz\/wp-content\/uploads\/2021\/02\/4-37.18.pdf\"><strong>T\u00e9l\u00e9charger l&rsquo;article<img loading=\"lazy\" decoding=\"async\" class=\" wp-image-709 alignright\" style=\"margin-top: -10px; margin-bottom: -10px;\" src=\"\/wp-content\/uploads\/2014\/04\/p2.jpg\" alt=\"p2\" width=\"37\" height=\"35\" srcset=\"https:\/\/synthese.univ-annaba.dz\/wp-content\/uploads\/2014\/04\/p2.jpg 113w, https:\/\/synthese.univ-annaba.dz\/wp-content\/uploads\/2014\/04\/p2-24x24.jpg 24w, https:\/\/synthese.univ-annaba.dz\/wp-content\/uploads\/2014\/04\/p2-48x46.jpg 48w\" sizes=\"auto, (max-width: 37px) 100vw, 37px\" \/><\/strong><\/a><\/p>\n<\/div>\n<p><strong>R\u00e9sum\u00e9<\/strong><\/p>\n<p style=\"text-align: justify;\">L\u2019\u00e9tude s\u00e9dimentologique de la s\u00e9rie n\u00e9ritique carbonat\u00e9e du groupe oriental Constantinois est le but essentiel de ce travail. Elle est bas\u00e9e sur une \u00e9tude lithologique et une \u00e9tude p\u00e9trographique \u00e0 l\u2019aide des lames minces. Cette derni\u00e8re nous a permis de reconstituer les variations des milieux de d\u00e9p\u00f4ts et de d\u00e9finir les diff\u00e9rents ph\u00e9nom\u00e8nes diag\u00e9n\u00e9tiques ayant affect\u00e9es ces formations et les conditions pal\u00e9o environnementaux du secteur \u00e9tudi\u00e9. La s\u00e9rie C\u00e9nomano-Albienne dans les deux flancs du Djebel Grar est essentiellement constitu\u00e9e de formations calcaires et dolomies sur lesquelles nos lames minces ont \u00e9t\u00e9 r\u00e9alis\u00e9es. L\u2019interpr\u00e9tation p\u00e9trographique a d\u00e9cel\u00e9 la pr\u00e9sence des microfaci\u00e8s qui correspondent \u00e0 des d\u00e9p\u00f4ts de la plate-forme externe et de la plate-forme interne et on distingue par ordre : Domaine distal de plateforme ouverte, domaine proximal moins ouvert, domaine peu profond calme partiellement agit\u00e9, domaine tr\u00e8s peu profond, peu agit\u00e9 a \u00e9nergie mod\u00e9r\u00e9.<\/p>\n<p><strong>Mots-cl\u00e9s<\/strong><\/p>\n<p>\u00e9tude s\u00e9dimentologique, s\u00e9rie n\u00e9ritique, c\u00e9nomano-albien, formations carbonat\u00e9es, milieu de d\u00e9p\u00f4t.<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Num\u00e9ro de la revue: Volume 26 , Num\u00e9ro 1 Manal Bouchama*&amp; Fella Assassi D\u00e9partement de G\u00e9ologie, Universit\u00e9 Badji-Mokhtar, BP 12, Annaba 23000, Alg\u00e9rie. &nbsp; T\u00e9l\u00e9charger l&rsquo;article R\u00e9sum\u00e9 L\u2019\u00e9tude s\u00e9dimentologique de la s\u00e9rie n\u00e9ritique carbonat\u00e9e du groupe oriental Constantinois est le &hellip; <a href=\"https:\/\/synthese.univ-annaba.dz\/?p=8336\">Lire la suite <span class=\"meta-nav\">&raquo;<\/span><\/a><\/p>\n","protected":false},"author":5,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1384],"tags":[1397,1395,1398,1399,1396],"class_list":["post-8336","post","type-post","status-publish","format-standard","hentry","category-synthese-vol-26-numero-1","tag-cenomano-albien","tag-etude-sedimentologique","tag-formations-carbonatees","tag-milieu-de-depot","tag-serie-neritique"],"_links":{"self":[{"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=\/wp\/v2\/posts\/8336","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=8336"}],"version-history":[{"count":2,"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=\/wp\/v2\/posts\/8336\/revisions"}],"predecessor-version":[{"id":8339,"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=\/wp\/v2\/posts\/8336\/revisions\/8339"}],"wp:attachment":[{"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=8336"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=8336"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/synthese.univ-annaba.dz\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=8336"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}