{"id":110237,"date":"2023-10-06T14:12:00","date_gmt":"2023-10-06T11:12:00","guid":{"rendered":"https:\/\/milliycha.uz\/?p=110237"},"modified":"2023-10-06T14:12:03","modified_gmt":"2023-10-06T11:12:03","slug":"ofiolitlar","status":"publish","type":"post","link":"https:\/\/milliycha.uz\/ru\/ofiolitlar\/","title":{"rendered":"Ofiolitlar"},"content":{"rendered":"\n<p>Ofiolitlar (Yunoncha ophis \u2014 ilon va lithos \u2014 tosh) \u2014 o&#8217;ta asosli va asosli intruziv (dunit, peridodit, piroksenit, gabbro), effuziv (giberbazitlar) va cho&#8217;kindi (aksari chuqur suv yotqiziqlari) tog&#8217; jinslarining birgalikda uchraydigan majmui. Ofiolitlar tushunchasini fanga dastlab 1905 yilda shveytsariyalik olim G. Shteynman kiritgan. Burmalangan oblastlarning Ofiolitlar okean osti yer po&#8217;stining o&#8217;tmish geologik davrda tektonik harakatlar natijasida qit&#8217;alar chetiga kelib qolgan relikti deb taxmin qilinadi. Odatda, serpentinlashgan ultrabazitlar yuqori mantiyaning bir qismi, gabbroidlar \u2014 &#171;basalt qatlami&#187;, effuziv-cho&#8217;kindi qatlamlar esa hozirgi okean osti yer po&#8217;stining &#171;birinchi&#187; va &#171;ikkinchi&#187; qatlamlaridan iborat. Bu tartibning o&#8217;zgarishi ko&#8217;pincha tektonik jarayonlar bilan bog&#8217;liq bo&#8217;lib, o&#8217;ziga xos geologik formasiya (serpentinli melanj)ni tashkil etadi. Ofiolitlar Yer sharining bir yo&#8217;nalishdagi burmali strukturalari uchun xos. Ofiolitlar ayrim hollarda gorizontal yo&#8217;nalishda katta masofalarga siljigan, ba&#8217;zan ag&#8217;darilgan. Ofiolitlarni tadqiq etish ofiolitli tog&#8217;jinslari bilan genetik bog&#8217;liq bo&#8217;lgan konlar (xrom, nikel, platina, oltin, simob va boshqalar)ni aniqlash va yer po&#8217;stining rivojlanishini o&#8217;rganishda katta ahamiyatga ega.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Ofiolitlar (Yunoncha ophis \u2014 ilon va lithos \u2014 tosh) \u2014 o&#8217;ta asosli va asosli intruziv (dunit, peridodit, piroksenit, gabbro), effuziv (giberbazitlar) va cho&#8217;kindi (aksari chuqur suv yotqiziqlari) tog&#8217; jinslarining birgalikda &hellip; <a href=\"https:\/\/milliycha.uz\/ru\/ofiolitlar\/\" 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":[225],"tags":[],"class_list":["post-110237","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-o-harfi-2","entry"],"translation":{"provider":"WPGlobus","version":"3.0.2","language":"ru","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\/ru\/wp-json\/wp\/v2\/posts\/110237","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/comments?post=110237"}],"version-history":[{"count":1,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts\/110237\/revisions"}],"predecessor-version":[{"id":110255,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts\/110237\/revisions\/110255"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/media\/99837"}],"wp:attachment":[{"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/media?parent=110237"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/categories?post=110237"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/tags?post=110237"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}