{"id":10909,"date":"2023-05-10T09:20:00","date_gmt":"2023-05-10T01:20:00","guid":{"rendered":"https:\/\/230411wadmp3.adwebcloud.com\/granite\/"},"modified":"2023-07-08T23:51:24","modified_gmt":"2023-07-08T15:51:24","slug":"granite","status":"publish","type":"post","link":"https:\/\/whitemarblegranite.com\/fi\/granite\/","title":{"rendered":"graniitti"},"content":{"rendered":"<p>Graniitti on intruusiokivi happamassa (SiO<sub>2<\/sub>&gt;66%) magmaattinen kivi. T\u00e4m\u00e4 on t\u00e4m\u00e4n luokan yleisin kivilaji, joka on useimmiten vaalean lihanpunaista, vaaleanharmaata ja luonnonvalkoista. Keskikarkea, hienorakeinen rakenne, lohkarerakenne. On my\u00f6s laikkumaisia rakenteita, pallomaisia rakenteita, gneissim\u00e4isi\u00e4 rakenteita ja niin edelleen.<\/p>\n<p><\/p>\n<p>P\u00e4\u00e4mineraalit ovat kvartsi, kalimaas\u00e4lp\u00e4 ja hapan plagioklaasi, ja sekund\u00e4\u00e4rimineraalit ovat biotiitti, sarviv\u00e4lke ja joskus pieni m\u00e4\u00e4r\u00e4 pyrokseenia. Lis\u00e4mineraaleja on monenlaisia, yleisimpi\u00e4 ovat magnetiitti, sfeeni, zirkoni, apatiitti, turmaliini, fluoriitti ja niin edelleen. Kvartsipitoisuus on suurin eri magmaattisten kivien joukossa, ja sen pitoisuus voi vaihdella 20-50%:n v\u00e4lill\u00e4, ja muutamat voivat saavuttaa 50-60%:n pitoisuuden.&nbsp;<\/p>\n<p><\/p>\n<p>Kalimaas\u00e4lp\u00e4pitoisuus on yleens\u00e4 suurempi kuin plagioklaasipitoisuus, ja n\u00e4iden kahden pitoisuuden v\u00e4linen suhde on usein sellainen, ett\u00e4 kalimaas\u00e4lp\u00e4\u00e4 on kaksi kolmasosaa koko maas\u00e4lv\u00e4st\u00e4, plagioklaasia on yksi kolmasosa, ja kalimaas\u00e4lp\u00e4\u00e4 on enemm\u00e4n graniitissa. Se on vaalean lihanpunaista, mutta my\u00f6s harmaata ja harmaata.<\/p>","protected":false},"excerpt":{"rendered":"<p>Granite is an intrusive rock in acidic (SiO2&gt;66%) magmatic rock. This is the most common type of rock in this category, mostly light flesh red, light gray, and off-white. Medium-coarse, fine-grained structure, block structure. There are also patchy structures, spherical structures, gneiss-like structures and so on. The main minerals are quartz, potash feldspar and acid [&hellip;]<\/p>\n","protected":false},"author":6,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[24],"tags":[],"class_list":["post-10909","post","type-post","status-publish","format-standard","hentry","category-knowledge"],"acf":[],"_links":{"self":[{"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/posts\/10909","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/comments?post=10909"}],"version-history":[{"count":0,"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/posts\/10909\/revisions"}],"wp:attachment":[{"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/media?parent=10909"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/categories?post=10909"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/whitemarblegranite.com\/fi\/wp-json\/wp\/v2\/tags?post=10909"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}