{"id":22373,"date":"2020-05-03T00:10:15","date_gmt":"2020-05-03T00:10:15","guid":{"rendered":"https:\/\/www.sohag-univ.edu.eg\/facsci\/?p=22373"},"modified":"2020-05-03T00:11:32","modified_gmt":"2020-05-03T00:11:32","slug":"%d8%a7%d9%84%d9%81%d8%b1%d9%82%d8%a9-%d8%a7%d9%84%d8%ab%d8%a7%d9%84%d8%ab%d8%a9-%d8%b5%d8%ae%d9%88%d8%b1%d8%b1%d8%b3%d9%88%d8%a8%d9%8a%d8%a9316%d8%ac-%d8%a3-%d8%af-%d8%aa%d9%88%d9%81%d9%8a%d9%82","status":"publish","type":"post","link":"https:\/\/sci.sohag-univ.edu.eg\/main\/%d8%a7%d9%84%d9%81%d8%b1%d9%82%d8%a9-%d8%a7%d9%84%d8%ab%d8%a7%d9%84%d8%ab%d8%a9-%d8%b5%d8%ae%d9%88%d8%b1%d8%b1%d8%b3%d9%88%d8%a8%d9%8a%d8%a9316%d8%ac-%d8%a3-%d8%af-%d8%aa%d9%88%d9%81%d9%8a%d9%82\/","title":{"rendered":"\u0627\u0644\u0641\u0631\u0642\u0629 \u0627\u0644\u062b\u0627\u0644\u062b\u0629 \u0635\u062e\u0648\u0631\u0631\u0633\u0648\u0628\u064a\u0629316\u062c \u0623.\u062f\/ \u062a\u0648\u0641\u064a\u0642 \u0645\u062d\u0645\u062f \u0645\u0647\u0631\u0627\u0646"},"content":{"rendered":"<table width=\"540\">\n<tbody>\n<tr>\n<td dir=\"ltr\" style=\"text-align: center;\" width=\"540\">1-Coarse grained terrigenous rocks: classifications and depositional environments<\/td>\n<\/tr>\n<tr dir=\"ltr\">\n<td style=\"text-align: center;\" width=\"540\">2- Algal laminites, stromatolites and oncolitic carbonates<\/td>\n<\/tr>\n<tr dir=\"ltr\">\n<td style=\"text-align: center;\" width=\"540\">3-Provenance, petrography and tectonic settings of medium grained clastic rocks<\/td>\n<\/tr>\n<tr dir=\"ltr\">\n<td style=\"text-align: center;\" width=\"540\">4- Non-marine carbonates: types and depositional environments<\/td>\n<\/tr>\n<tr dir=\"ltr\">\n<td style=\"text-align: center;\" width=\"540\">5-Dolomites and models of dolomitization<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n","protected":false},"excerpt":{"rendered":"<p>1-Coarse grained terrigenous rocks: classifications and depositional environments 2- Algal laminites, stromatolites and oncolitic carbonates 3-Provenance, petrography and tectonic settings of medium grained clastic rocks 4- Non-marine carbonates: types and depositional environments 5-Dolomites and models of dolomitization<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"zakra_page_container_layout":"customizer","zakra_page_sidebar_layout":"customizer","zakra_remove_content_margin":false,"zakra_sidebar":"customizer","zakra_transparent_header":"customizer","zakra_logo":0,"zakra_main_header_style":"default","zakra_menu_item_color":"","zakra_menu_item_hover_color":"","zakra_menu_item_active_color":"","zakra_menu_active_style":"","zakra_page_header":true,"footnotes":""},"categories":[1],"tags":[],"class_list":["post-22373","post","type-post","status-publish","format-standard","hentry","category-1"],"rttpg_featured_image_url":null,"rttpg_author":{"display_name":"admin","author_link":"https:\/\/sci.sohag-univ.edu.eg\/main\/author\/admin\/"},"rttpg_comment":0,"rttpg_category":"<a href=\"https:\/\/sci.sohag-univ.edu.eg\/main\/category\/%d8%a7%d8%ae%d8%a8%d8%a7%d8%b1-%d9%82%d8%b3%d9%85-%d8%a7%d9%84%d9%81%d9%8a%d8%b2%d9%8a%d8%a7%d8%a1\/\" rel=\"category tag\">\u0627\u062e\u0628\u0627\u0631 \u0642\u0633\u0645 \u0627\u0644\u0641\u064a\u0632\u064a\u0627\u0621<\/a>","rttpg_excerpt":"1-Coarse grained terrigenous rocks: classifications and depositional environments 2- Algal laminites, stromatolites and oncolitic carbonates 3-Provenance, petrography and tectonic settings of medium grained clastic rocks 4- Non-marine carbonates: types and depositional environments 5-Dolomites and models of dolomitization","_links":{"self":[{"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/posts\/22373","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/comments?post=22373"}],"version-history":[{"count":1,"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/posts\/22373\/revisions"}],"predecessor-version":[{"id":22374,"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/posts\/22373\/revisions\/22374"}],"wp:attachment":[{"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/media?parent=22373"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/categories?post=22373"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/sci.sohag-univ.edu.eg\/main\/wp-json\/wp\/v2\/tags?post=22373"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}