{"id":45,"date":"2024-04-04T06:11:38","date_gmt":"2024-04-04T03:11:38","guid":{"rendered":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/porfuriit\/"},"modified":"2024-04-04T06:13:07","modified_gmt":"2024-04-04T03:13:07","slug":"porfuriit","status":"publish","type":"page","link":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/porfuriit\/","title":{"rendered":"Porf\u00fcriit"},"content":{"rendered":"<p>\n\t<font face=\"Arial\"><font style=\"medium;font-style:normal;font-weight:400;letter-spacing:normal;text-align:start;text-indent:0px;text-transform:none\"><b>Porf\u00fcriitide<\/b>\u00a0p\u00f5himass on v\u00e4ga peeneteraline, tihe, palja silmaga sageli mitteeraldatavate kristallikestega (foto 1). Valdava mineraali j\u00e4rgi eristatakse plagioklass-, biotiit- ja amfiboolporfuriite.<\/font><\/font>\n<\/p>\n<p>\n\t<font face=\"Arial\">Eesti r\u00e4ndkivide seas on tuntumaks porf\u00fcriidiks labradorporf\u00fcriidid, rohekasmustad kivimid, milles esinevad suured, kuni 2 cm l\u00e4bim\u00f5\u00f5duga tumerohekad plaatja kujuga plagioklassi kristallid.<\/font>\n<\/p>\n<p>\n\t<img loading=\"lazy\" decoding=\"async\" width=\"117\" height=\"120\" class=\"alignnone wp-image-268\" src=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/431\/porfyriit1a.jpg\" title=\"porfyriit1a.jpg\" alt=\"porfyriit\"><br><font face=\"Arial\">Foto 1. Porf\u00fcriit, Waldbl\u00f6ckelheim<\/font>\n<\/p>\n<p style=\"text-align:start\">\n\t<br><span><span style=\"color:#000000\"><span><span style=\"font-style:normal\"><span><span><span style=\"font-weight:400\"><span style=\"letter-spacing:normal\"><span><span style=\"text-transform:none\"><span><span><span><span><span>Koostanud ja fotografeerinud \u00a9 2003 Mare Isakar<\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Porf\u00fcriitide\u00a0p\u00f5himass on v\u00e4ga peeneteraline, tihe, palja silmaga sageli mitteeraldatavate kristallikestega (foto 1). Valdava mineraali j\u00e4rgi eristatakse plagioklass-, biotiit- ja amfiboolporfuriite. Eesti r\u00e4ndkivide seas on tuntumaks porf\u00fcriidiks labradorporf\u00fcriidid, rohekasmustad kivimid, milles esinevad suured, kuni 2 cm l\u00e4bim\u00f5\u00f5duga tumerohekad plaatja kujuga plagioklassi &#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-45","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/45","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=45"}],"version-history":[{"count":1,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/45\/revisions"}],"predecessor-version":[{"id":811,"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/pages\/45\/revisions\/811"}],"wp:attachment":[{"href":"https:\/\/sisu.ut.ee\/mineraalid-ja-kivimid\/wp-json\/wp\/v2\/media?parent=45"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}