{"id":106340,"date":"2023-09-15T13:05:11","date_gmt":"2023-09-15T10:05:11","guid":{"rendered":"https:\/\/milliycha.uz\/?p=106340"},"modified":"2023-09-15T13:05:14","modified_gmt":"2023-09-15T10:05:14","slug":"rifey","status":"publish","type":"post","link":"https:\/\/milliycha.uz\/kr\/rifey\/","title":{"rendered":"Rifey"},"content":{"rendered":"\n<p>Rifey (lotincha Ri phaei montes \u2014 Rifey tog&#8217;lari; qadimgi geograflar Ural tog&#8217;larini ba&#8217;zan shunday ataganlar) \u2014 kechki pjembriyga mansub yirik stratigrafik bo&#8217;linma. Geologik yoshi 1650\u2014 570 million yil bo&#8217;lgan, kam o&#8217;zgarishga uchragan tog&#8217; jinslaridan iborat; kembriy davri bilan almashgan. Rifey 1945 yil rus geologi N.S. Shatskiy tomonidan Janubiy Uralda aniqlangan. Taxminan yuqori proterozoyga muvofiq keladi. Rifey tarkibida 4 ta bo&#8217;linma mavjud: quyi, o&#8217;rta, yuqori va vend. So&#8217;nggi bo&#8217;linmaga mustaqil majmua sifatida qaraladi va ko&#8217;pincha terminal Rifey, yoki vendomi deb ataladi. Shu 4 bo&#8217;linmaning har biri tarkibida Rifey yotqiziqlarini bo&#8217;limlarga ajratish va korrelyatsiya qilishda asos bo&#8217;ladigan ko&#8217;k-yashil suvo&#8217;tlar qoldiqlari (stromatolitlar)ning o&#8217;ziga xos majmuini ko&#8217;rish mumkin. Rifeyning dengiz va quruqlikdagi yotqiziklari barcha materikda tarqalgan. Platformalar Rifeyda paleozoydagiga nisbatan kichiroq maydonni egallagan. Ular yassi quruqlikdan iborat bo&#8217;lib, ustidagi qadimgi jinslar yuvilib ketgan. Nuragan jinslar esa bukilmalarda to&#8217;plana borgan. Geosinklinal sistemalarning tashqi bukilmalarida qumtoshli jinslar bilan birga gilli karbonatli, ba&#8217;zan flish (Tyanshanda) yotqiziqlari vujudga kelgan. Okean tubidagi yer pusti ichki bukilmalarida suv osti vulkan mahsulotlari yig&#8217;ilgan. Rifey oxirida keng maydonlarda motsslar yotqizilgan. Rifeyda arid (quruq) ikdim bo&#8217;lganligi uchun qizil yotqiziqlar to&#8217;plangan. Biroq yuqori Rifeyning 2-yarmida va terminal Rifeyda ko&#8217;p o&#8217;lkalarda muzlik yotqiziqlari uchraydi. Rifeyning kabonatli jinslarida ko&#8217;plab stromatolitlar mavjud. Qatlamlarni ajratishda mikrofitolitlar muhim ahamiyatga ega. Rifey cho&#8217;kindilarida stratigrafik ahamiyatga ega bo&#8217;lgan akritarxlar mavjud. Rifeyda umurtqasizlarning dastlabki tiplari paydo bo&#8217;lib, erta paleozoyda ravnaq topgan. Rifeyning yuqori qismida skeletsiz ko&#8217;p hujayrali hayvonlar uchraydi. Halqali chuvalchanglar yaxshi namoyon bo&#8217;lgan. Foydali qazilmalardan Rifey cho&#8217;kindilarida temir rudasi, fosforitlar, ayrim joylarda qo&#8217;rg&#8217;oshin-rux, Ekvatorial Afrikada mis, kobalt va uran rudalari mavjud. Sibir platformasida terminal Rifeyda gazkondensatlar va neft uyumlari aniqlangan.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Rifey (lotincha Ri phaei montes \u2014 Rifey tog&#8217;lari; qadimgi geograflar Ural tog&#8217;larini ba&#8217;zan shunday ataganlar) \u2014 kechki pjembriyga mansub yirik stratigrafik bo&#8217;linma. Geologik yoshi 1650\u2014 570 million yil bo&#8217;lgan, kam &hellip; <a href=\"https:\/\/milliycha.uz\/kr\/rifey\/\" 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":[214],"tags":[],"class_list":["post-106340","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-r-harfi","entry"],"translation":{"provider":"WPGlobus","version":"3.0.2","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\/106340","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=106340"}],"version-history":[{"count":1,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/106340\/revisions"}],"predecessor-version":[{"id":106345,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/106340\/revisions\/106345"}],"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=106340"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/categories?post=106340"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/tags?post=106340"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}