{"id":131470,"date":"2024-06-10T20:31:51","date_gmt":"2024-06-10T17:31:51","guid":{"rendered":"https:\/\/milliycha.uz\/?p=131470"},"modified":"2024-06-10T20:31:55","modified_gmt":"2024-06-10T17:31:55","slug":"tektonik-bukilmalar","status":"publish","type":"post","link":"https:\/\/milliycha.uz\/kr\/tektonik-bukilmalar\/","title":{"rendered":"TEKTONIK BUKILMALAR"},"content":{"rendered":"\n<p>TEKTONIK BUKILMALAR &#8211; Er po&#8217;stining tektonik harakatlar natijasida vujudga kelgan chiziq shaklidagi har qanday pasayishi yoki bukilishining umumiy nomi. T.b. Er pusti evolyusiyasining turli davrlarida har xil kuchlar ta&#8217;siri ostida paydo bo&#8217;ladigan ko&#8217;pgina turlitumanlik bilan tavsiflanadi. Ular, odatda, o&#8217;zlari bilan bir vaqtda paydo bo&#8217;lgan tektonik ko&#8217;tarilmalar bilan bog&#8217;liq bo&#8217;ladi. T. b. orasida shartli ravishda bir necha guruhlar ajratilishi mumkin: geosin klinalli T.b. \u2014 chuqur bukilishning tor zonalari bo&#8217;lib, cho&#8217;kindi va vulkanogen jinslarning kalin katlami bilan to&#8217;lgan va keyinchalik burmalanishga uchragan (q. Geosinklinal); ular, odatda, Er po&#8217;stining kuchli cho&#8217;zilishi sharoitida vujudga keladi. Uzun novsimon geosinklinal bukilmalar ba&#8217;zan tektonik troglar deb ataladi (N. S. Shatskiy, 1946). Odatda, ularning o&#8217;rnida burmalanish jarayonida yirik sinklinoriylar shakllanadi. Burmalangan oblastlarning ichki (evgeosinklinal) zonasida joylashgan geosinklinal T.b. okean osti er pusti tipida rivojlangan (mas., Uraldagi Magnitogorsk, Tagil bukilmalari); burmalangan oblastlarning tashki (miogeosinklinal) zonasida joylashgan geosinklinal T.b. kontinental (qurukdik) Er po&#8217;stining tagiga joylashadi. Chekka yoki old T.b. tog&#8217;lar zanjirining o&#8217;sish oldi tomondan siqilish sharoitida platformalar chetida tog&#8217;hosil bo&#8217;lish va burmalanish epoxasida vujudga keladi (mas., Uraloldi, Alo&#8217;yuldi, Mesopotamiya va b.) va ularning emirilish mahsuloti, asosan, molasslar bilan tuldiriladi; ularning bukilishi ma&#8217;lum miqdorda yondosh burmali tog&#8217;larning ko&#8217;tarilishini ta&#8217;minlaydi. Geosinklinal rivojlanishining orogen etapida burmalangan oblastlarning orqa qismida tog&#8217;lararo bukilma hosil bo&#8217;ladi, ular ko&#8217;tarilmalar (tog&#8217;tizmalari) oralig&#8217;idagi tektonik depressiyalardan iborat va chekka T.b. singari molasslar bilan to&#8217;lgan. Platforma ichki T.b. ham mavjud bo&#8217;lib, bular orasida riftli bukilmalar qad. avlokogenlar kabi alohida o&#8217;rin egallaydi. Epiplatformali orogenez jarayonida molass yotqiziklari bilan to&#8217;ldirilgan, lekin vulkanizm hodisasisiz tog&#8217;oldi T. b. vujudga keladi. T.b. oldingi bu-kilmalar o&#8217;rnida katta tanaffussiz vaqt davomida paydo bo&#8217;lgan va ancha qad. strukturalarda uzoq tanaffusdan keyin vujudga kelgan, nomuvofiq holda yotgan qoplamali bukilmalarga bo&#8217;linadi. T.b. qiya sinklinal, sinklinoriy, grabenlar shaklida bo&#8217;ladi; ba&#8217;zi hollarda T.b.ning cho&#8217;kindi jinslari tektonik qoplam ko&#8217;rinishida chetga siqib chiqariladi.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>TEKTONIK BUKILMALAR &#8211; Er po&#8217;stining tektonik harakatlar natijasida vujudga kelgan chiziq shaklidagi har qanday pasayishi yoki bukilishining umumiy nomi. T.b. Er pusti evolyusiyasining turli davrlarida har xil kuchlar ta&#8217;siri ostida &hellip; <a href=\"https:\/\/milliycha.uz\/kr\/tektonik-bukilmalar\/\" 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-131470","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\/131470","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=131470"}],"version-history":[{"count":1,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/131470\/revisions"}],"predecessor-version":[{"id":131488,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/posts\/131470\/revisions\/131488"}],"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=131470"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/categories?post=131470"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/milliycha.uz\/kr\/wp-json\/wp\/v2\/tags?post=131470"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}