{"id":63,"date":"2024-04-04T06:11:40","date_gmt":"2024-04-04T03:11:40","guid":{"rendered":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/suvakivimid\/"},"modified":"2024-04-04T06:13:06","modified_gmt":"2024-04-04T03:13:06","slug":"suvakivimid","status":"publish","type":"page","link":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/suvakivimid\/","title":{"rendered":"S\u00fcvakivimid"},"content":{"rendered":"<p>\n\t<b>Intrusiivsed ehk suvakivimid<\/b>\u00a0tekivad s\u00fcgavustest p\u00e4rit magma jahtumisel ja tardumisel maakoores. S\u00fcvakivimid tulevad n\u00e4htavale vaid p\u00e4rast nendel lasuvate kivimite kulumist ja \u00e4rakannet. Magma jahtumisel hakkavad sellest kristalliseeruma mineraalid. S\u00fcvakivimite alajaotusena eraldatakse v\u00e4lja veel\u00a0<b>poolsuvakivimid<\/b>\u00a0ja l\u00f5hesid t\u00e4itvad\u00a0<b>soonkivimid<\/b>.\n<\/p>\n<p>\n\t<b>Poolsuvakivimid<\/b>\u00a0on tardunud suhteliselt v\u00e4iksema r\u00f5hu ja kiirema jahtumise tingimustes (v\u00e4iksemas s\u00fcgavuses). Sellest tingitult on nad peeneteralise ehitusega.\n<\/p>\n<p>\n\t<b>Soonkivimid<\/b>\u00a0tekivad l\u00f5hedes magma j\u00e4\u00e4klahustest. Neid iseloomustavad suured kristallid (l\u00e4bim\u00f5\u00f5t v\u00f5ib ulatuda kuni mitmek\u00fcmne sentimeetrini).\n<\/p>\n<p>\n\tT\u00fc\u00fcpilisteks s\u00fcvakivimiteks on\u00a0<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/graniit\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/graniit\" target=\"_blank\" title=\"\" rel=\"noopener\">graniit<\/a>,\u00a0<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/dioriit\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/dioriit\" target=\"_blank\" title=\"\" rel=\"noopener\">dioriit<\/a>\u00a0ja\u00a0<a data-url=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/gabro\" href=\"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/gabro\" target=\"_blank\" title=\"\" rel=\"noopener\">gabro<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Intrusiivsed ehk suvakivimid\u00a0tekivad s\u00fcgavustest p\u00e4rit magma jahtumisel ja tardumisel maakoores. S\u00fcvakivimid tulevad n\u00e4htavale vaid p\u00e4rast nendel lasuvate kivimite kulumist ja \u00e4rakannet. Magma jahtumisel hakkavad sellest kristalliseeruma mineraalid. S\u00fcvakivimite alajaotusena eraldatakse v\u00e4lja veel\u00a0poolsuvakivimid\u00a0ja l\u00f5hesid t\u00e4itvad\u00a0soonkivimid. Poolsuvakivimid\u00a0on tardunud suhteliselt v\u00e4iksema r\u00f5hu ja &#8230;<\/p>\n","protected":false},"author":226,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"inline_featured_image":false,"footnotes":""},"class_list":["post-63","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/63","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/users\/226"}],"replies":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/comments?post=63"}],"version-history":[{"count":1,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/63\/revisions"}],"predecessor-version":[{"id":792,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/63\/revisions\/792"}],"wp:attachment":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/media?parent=63"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}