{"id":117534,"date":"2024-05-08T22:03:29","date_gmt":"2024-05-08T19:03:29","guid":{"rendered":"https:\/\/milliycha.uz\/?p=117534"},"modified":"2024-05-08T22:03:33","modified_gmt":"2024-05-08T19:03:33","slug":"tog-jinslarining-burmalanishi","status":"publish","type":"post","link":"https:\/\/milliycha.uz\/kr\/tog-jinslarining-burmalanishi\/","title":{"rendered":"Tog&#8217; jinslarining burmalanishi"},"content":{"rendered":"\n<p>Tog&#8217; jinslarining burmalanishi, burmalanishning hosil bo&#8217;lishi \u2014tektonik deformasiyalar natijasida tog&#8217;jinslari katlamlarining ezilib, burmalanish jarayoni. Burmalar majmuasi shakli, kelib chiqishi va hosil bo&#8217;lishining kinematik sharoitlariga qarab farqlanadi. T.j.b. morfologik belgilarga qarab to&#8217;liq, golomorfli yoki uzun, ingichka burmalardan tashkil topgan, qavariq (antiklinal) va botiq (sinklinal) burmalangan zonalarni muntazam to&#8217;ldirib turuvchi chizikdi (alpinotipli); uzuqyulukli yoki alohida, tarqoq, ko&#8217;proq antiklinal burmalarga yakin turli shakldagi (vallar, gumbazlar, noto&#8217;g&#8217;ri ko&#8217;rinishli ko&#8217;tarilmalar) to&#8217;g&#8217;ri yotgan qatlamlar maydonlari bilan bo&#8217;lingan guruhlardan tashkil topgan idiomorfli; oralik, burmalanishli va b. tiplarga bo&#8217;linadi. To&#8217;liq burmalanishda hududning qamma maydoni antiklinal va sinklinal burmalar bilan band bo&#8217;lib, gorizontal katlamlar uchramaydi. Unda, asosan, surilish va ushalish, tog&#8217;jinslarining jipslashishi va metamorfizmi sodir bo&#8217;ladi. Uzuqyuluq burmalanishga braxiantiklinal va braxisinklinallar, ko&#8217;tarilmalar, gumbazlar, diapir burma va b. kiradi. Ularda tik tektonik buzilishlar ko&#8217;p uchraydi. Oraliq burmalanishlar 2 xil: qirrasimon va sandik,Simon bo&#8217;ladi. Qirrasimon burmalanishda jarlik, siqiq antiklinal va keng tekis sinklinallar navbatmanavbat keladi, tog oldi bukilmalarida uchraydi. Sandiqsimon burmalanish sandiqsimon antiklinal va sinklinallardan iborat. Turli davrlarda hosil bo&#8217;lgan turli yoshdagi burmalanishlar ma&#8217;lum. Mas., Baykal (tokembriy oxiri \u2014 kembriy boshi), Kaledon (quyi paleozoy oxirida), gersin (yuqori paleozoyda), kimmeriy yoki Tinch okean (yuqori yura va bur davrlarida) va Alp (kaynozoyda) burmalanishlari. T.j.b.ni o&#8217;rganish faqat nazariy emas, balki amaliy ahamiyatga ega, chunki burmali deformasiyalar foydali qazilmalar yotishining tavsifiga va kontsentrasiyasiga ta&#8217;sir ko&#8217;rsatadi. T.j.b. paytida neft, gaz va ba&#8217;zi bir ruda konlari hosil bo&#8217;ladi va to&#8217;planadi.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tog&#8217; jinslarining burmalanishi, burmalanishning hosil bo&#8217;lishi \u2014tektonik deformasiyalar natijasida tog&#8217;jinslari katlamlarining ezilib, burmalanish jarayoni. Burmalar majmuasi shakli, kelib chiqishi va hosil bo&#8217;lishining kinematik sharoitlariga qarab farqlanadi. T.j.b. morfologik belgilarga qarab &hellip; <a href=\"https:\/\/milliycha.uz\/kr\/tog-jinslarining-burmalanishi\/\" 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":[187],"tags":[],"class_list":["post-117534","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-t-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\/117534","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=117534"}],"version-history":[{"count":1,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/117534\/revisions"}],"predecessor-version":[{"id":117540,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/117534\/revisions\/117540"}],"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=117534"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/categories?post=117534"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/tags?post=117534"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}