{"id":22192,"date":"2020-04-30T22:33:02","date_gmt":"2020-04-30T22:33:02","guid":{"rendered":"https:\/\/www.sohag-univ.edu.eg\/facsci\/?p=22192"},"modified":"2020-04-30T22:50:21","modified_gmt":"2020-04-30T22:50:21","slug":"%d8%a8%d8%b5%d8%b1%d9%8a%d8%a7%d8%aa-%d8%a7%d9%84%d9%85%d8%b9%d8%a7%d8%af%d9%86-%d9%88-%d8%b9%d9%84%d9%85-%d8%a7%d9%84%d9%85%d8%b9%d8%a7%d8%af%d9%86112%d8%ac%d8%a7%d9%84%d8%a7%d9%88%d9%84%d9%89","status":"publish","type":"post","link":"https:\/\/sci.sohag-univ.edu.eg\/main\/%d8%a8%d8%b5%d8%b1%d9%8a%d8%a7%d8%aa-%d8%a7%d9%84%d9%85%d8%b9%d8%a7%d8%af%d9%86-%d9%88-%d8%b9%d9%84%d9%85-%d8%a7%d9%84%d9%85%d8%b9%d8%a7%d8%af%d9%86112%d8%ac%d8%a7%d9%84%d8%a7%d9%88%d9%84%d9%89\/","title":{"rendered":"\u0628\u0635\u0631\u064a\u0627\u062a \u0627\u0644\u0645\u0639\u0627\u062f\u0646 \u0648 \u0639\u0644\u0645 \u0627\u0644\u0645\u0639\u0627\u062f\u0646112\u062c\t\u0627\u0644\u0627\u0648\u0644\u0649\t\u0627\u0644\u062c\u064a\u0648\u0644\u0648\u062c\u064a\u0627\t\u0627.\u062f\/ \u0631\u0645\u0636\u0627\u0646 \u0628\u062e\u064a\u0631 \u0648 \u062f\/ \u0627\u062d\u0645\u062f \u0639\u0628\u062f\u0627\u0644\u0631\u0634\u064a\u062f"},"content":{"rendered":"<p dir=\"ltr\" style=\"text-align: center;\">1- The polarizing microscope and silicate structures and mineral groups.<\/p>\n<p dir=\"ltr\" style=\"text-align: center;\">2- Interpretation of twinning under cross nicols and tectosilicate minerals.<\/p>\n<p dir=\"ltr\" style=\"text-align: center;\">3- Optical indicatrix of minerals and rock-forming minerals of igneous rocks.<\/p>\n<p dir=\"ltr\" style=\"text-align: center;\">4- Study of minerals coossed polars (nicols) and metamorphic minerals.<\/p>\n<p dir=\"ltr\" style=\"text-align: center;\">5- The study of minerals under convergent light and accessory minerals.<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p style=\"text-align: center;\">\n","protected":false},"excerpt":{"rendered":"<p>1- The polarizing microscope and silicate structures and mineral groups. 2- Interpretation of twinning under cross nicols and tectosilicate minerals. 3- Optical indicatrix of minerals and rock-forming minerals of igneous rocks. 4- Study of minerals coossed polars (nicols) and metamorphic minerals. 5- The study of minerals under convergent light and accessory minerals. &nbsp; &nbsp;<\/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-22192","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":1,"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- The polarizing microscope and silicate structures and mineral groups. 2- Interpretation of twinning under cross nicols and tectosilicate minerals. 3- Optical indicatrix of minerals and rock-forming minerals of igneous rocks. 4- Study of minerals coossed polars (nicols) and metamorphic minerals. 5- The study of minerals under convergent light and accessory minerals. &nbsp; 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