{"id":123178,"date":"2024-05-12T20:02:47","date_gmt":"2024-05-12T17:02:47","guid":{"rendered":"https:\/\/milliycha.uz\/?p=123178"},"modified":"2024-05-12T20:02:57","modified_gmt":"2024-05-12T17:02:57","slug":"kaolinlanish","status":"publish","type":"post","link":"https:\/\/milliycha.uz\/ru\/kaolinlanish\/","title":{"rendered":"Kaolinlanish"},"content":{"rendered":"\n<p>Kaolinlanish \u2014 gilli mine- rallar (asosan, dala shpatlari va slyu- dalar)ning o&#8217;zgarishi hisobiga kaolin yuzaga kelgan holda tog&#8217;jinslarining o&#8217;zgarishi. K. 2 xil sharoitda: alyumosi- likatlarga boy magmatik va metamorfik jinslarning nurashi (ekzogen) va past t-rali gidrotermal suvlarning alyumo- silikatlarga ta&#8217;sir qilishi (endogen) yo&#8217;li b-n sodir bo&#8217;ladi. Ekzogen K. Er tarixining toshko&#8217;mir, yura va uchlamchi davrlarida nam, subtropik iqlim sharo- itlarida yuz bergan. K. natijasida pay- do bo&#8217;lgan kaolinitning asosiy konlari xam shu davrga xos. Endogen K.da kaoli- nit alyumosilikatlar va b. minerallar- ning o&#8217;rnini egallab, ularning shakli va qiyofasiga o&#8217;tib, psevdomorfozalar hosil qiladi. Bu jarayon ko&#8217;proq rudali konlar atrofidagi tog&#8217;jinslari orasida bo&#8217;ladi. K. jarayoni oltingugurtli, kar- bonat angidridli va galoidli eritmalar hamda guminli kislotalar katnashuvi natijasida yuz beradi. O&#8217;zbekistonda K. juda keng tarqalgan, ayniqsa, rudali konlar atrofidagi tog&#8217;jinslarining o&#8217;zgarishi b-n bog&#8217;liq holda ko&#8217;p kuzati- ladi.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Kaolinlanish \u2014 gilli mine- rallar (asosan, dala shpatlari va slyu- dalar)ning o&#8217;zgarishi hisobiga kaolin yuzaga kelgan holda tog&#8217;jinslarining o&#8217;zgarishi. K. 2 xil sharoitda: alyumosi- likatlarga boy magmatik va metamorfik jinslarning &hellip; <a href=\"https:\/\/milliycha.uz\/ru\/kaolinlanish\/\" 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":[201],"tags":[],"class_list":["post-123178","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-k-harfi","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\/123178","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=123178"}],"version-history":[{"count":1,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts\/123178\/revisions"}],"predecessor-version":[{"id":123195,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/posts\/123178\/revisions\/123195"}],"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=123178"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/categories?post=123178"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/milliycha.uz\/ru\/wp-json\/wp\/v2\/tags?post=123178"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}