{"id":105389,"date":"2023-09-09T17:32:26","date_gmt":"2023-09-09T14:32:26","guid":{"rendered":"https:\/\/milliycha.uz\/?p=105389"},"modified":"2023-09-09T17:32:32","modified_gmt":"2023-09-09T14:32:32","slug":"sharqiy-yevropa-platformasi","status":"publish","type":"post","link":"https:\/\/milliycha.uz\/kr\/sharqiy-yevropa-platformasi\/","title":{"rendered":"Sharqiy yevropa platformasi"},"content":{"rendered":"\n<p>Sharqiy yevropa platformasi, rus platformasi, Yevropa platformasi \u2014 yirik platformalardan biri, yer po&#8217;stining qadimiy rifeygacha bo&#8217;lgan davriga mansub. Sharqiy va Shimoliy Yevropaning katta qismini egallab, Skandinaviya tog&#8217;laridan Uralgacha va Barents dengizidan qora hamda kaspiy dengizlarigacha cho&#8217;zilgan. Platforma chegarasi shimoli Sharq va shimolda Timan kryaji bo&#8217;ylab hamda Kola yarim oroli qirg&#8217;oqlaridan, Janubi g&#8217;arbda esa \u2014 O&#8217;rta Yevropa tekisligida Varshava yaqinidan, shimoli g&#8217;arbda Boltiq dengizi va Yutlandiya yarim orolining shimol qismidan o&#8217;tadi. Sharqiy yevropa platformasida rifeygacha bo&#8217;lgan burmalangan qadimiy kristalli zamin bilan uning ustida yotgan cho&#8217;kindi jinslar qoplami ajralib turadi. Zamin platformaning faqat shimoli g&#8217;arbida (Boltiq qalqoni) va Janubi g&#8217;arbidagina (Ukraina qalqoni) yer yuzasiga chiqib yotadi. Qolgan katta maydonda u cho&#8217;kindi yotqiziqlari bilan qoplangan. Sharqiy yevropa platformasining zaminida kuchli metamorflashgan va burmalangan cho&#8217;kindi hamda magmatik jinslar bo&#8217;lib, bu jinslar katta maydonlarda gneys va kristalli slaneslarga aylangan. Platforma zaminining aksari qismi (g&#8217;arbiy chekkasi bundan istisno) yuqori proterozoy boshlarida (1600 million yil oldin) shakllangan. Sharqiy yevropa platformasi tarixida 2 yirik davr ajralib turadi. 1-davr arxey, quyi va o&#8217;rta proterozoy davrlarini (3500\u2014 1600 million yil) o&#8217;z ichiga oladi, bunda kristalli zamin shakllangan; 2-davrda (yuqori proterozoydan antropogengacha) esa platformaning o&#8217;zi rivojlanib, cho&#8217;kindi qoplam va hozirgi struktura hosil bo&#8217;lgan. Paleozoy davrining oxirlarida Sharqiy yevropa platformasining strukturalari qayta tiklanishi natijasida yer sathining katta qismi qo&#8217;tarilgan. Bunga Sharqda sodir bo&#8217;lgan Ural-Tyanshan geosinklinal mintaqasidagi gersin davrining burmalanish harakati ta&#8217;sir ko&#8217;rsatgan. Zamindagi foydali qazilmalar: temir rudasi (Krivoy Rog havzasi, Kursk magnit anomaliyasi, Kiruna), nikel, mis, titan rudalari, slyudalar, pegmatitlar apatit va boshqalar cho&#8217;kindi qoplamda yonuvchi gaz va neft qatlamlari (Volga \u2014 Ural anteklizasi, Pripyat botig&#8217;i), tosh tuzi va kaliy tuzi konlari (Kama, Ural oldi, Pripyat botig&#8217;i), qazilma ko&#8217;mir (Lvov, Donesk, Moskva yoni havzalari), fosforit, boksit, qurilish xom ashyosi (ohaktosh, dolomit, gil va boshqalar) konlari, shuningdek, chuchuk va mineral suvlar bor.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Sharqiy yevropa platformasi, rus platformasi, Yevropa platformasi \u2014 yirik platformalardan biri, yer po&#8217;stining qadimiy rifeygacha bo&#8217;lgan davriga mansub. Sharqiy va Shimoliy Yevropaning katta qismini egallab, Skandinaviya tog&#8217;laridan Uralgacha va Barents &hellip; <a href=\"https:\/\/milliycha.uz\/kr\/sharqiy-yevropa-platformasi\/\" class=\"more-link\">Read More<\/a><\/p>\n","protected":false},"author":1,"featured_media":99837,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[211],"tags":[],"class_list":["post-105389","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-sh-harfi","entry"],"translation":{"provider":"WPGlobus","version":"3.0.0","language":"kr","enabled_languages":["uz","kr","ru"],"languages":{"uz":{"title":true,"content":true,"excerpt":false},"kr":{"title":false,"content":false,"excerpt":false},"ru":{"title":false,"content":false,"excerpt":false}}},"_links":{"self":[{"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/105389","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/comments?post=105389"}],"version-history":[{"count":1,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/105389\/revisions"}],"predecessor-version":[{"id":105396,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/105389\/revisions\/105396"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/media\/99837"}],"wp:attachment":[{"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/media?parent=105389"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/categories?post=105389"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/tags?post=105389"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}