{"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\/tr\/granite\/","title":{"rendered":"granit"},"content":{"rendered":"<p>Granit, asidik (SiO<sub>2<\/sub>&gt;66%) magmatik kaya\u00e7. Bu kategorideki en yayg\u0131n kaya t\u00fcr\u00fcd\u00fcr, \u00e7o\u011funlukla a\u00e7\u0131k et k\u0131rm\u0131z\u0131s\u0131, a\u00e7\u0131k gri ve kirli beyazd\u0131r. Orta-kaba, ince taneli yap\u0131, blok yap\u0131. Ayr\u0131ca yamal\u0131 yap\u0131lar, k\u00fcresel yap\u0131lar, gnays benzeri yap\u0131lar vb. de vard\u0131r.<\/p>\n<p><\/p>\n<p>Ana mineraller kuvars, potas feldispat ve asit plajiyoklazd\u0131r ve ikincil mineraller biyotit, hornblend ve bazen az miktarda piroksendir. Bir\u00e7ok aksesuar mineral t\u00fcr\u00fc vard\u0131r, yayg\u0131n olanlar manyetit, sfen, zirkon, apatit, turmalin, florit ve benzerleridir. Kuvars i\u00e7eri\u011fi \u00e7e\u015fitli magmatik kaya\u00e7lar aras\u0131nda en b\u00fcy\u00fck olan\u0131d\u0131r ve i\u00e7eri\u011fi 20-50% aras\u0131nda de\u011fi\u015febilir ve birka\u00e7\u0131 50-60%'ye ula\u015fabilir.&nbsp;<\/p>\n<p><\/p>\n<p>Potas feldspat i\u00e7eri\u011fi genellikle plajiyoklazdan daha fazlad\u0131r ve iki i\u00e7erik aras\u0131ndaki ili\u015fki genellikle potas feldspat\u0131n toplam feldspat\u0131n \u00fc\u00e7te ikisini olu\u015fturdu\u011fu, plajiyoklaz\u0131n \u00fc\u00e7te birini kaplad\u0131\u011f\u0131 ve potas feldspat\u0131n granitte daha fazla oldu\u011fu \u015feklindedir. A\u00e7\u0131k et k\u0131rm\u0131z\u0131s\u0131, ayn\u0131 zamanda gri ve gridir.<\/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\/tr\/wp-json\/wp\/v2\/posts\/10909","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/whitemarblegranite.com\/tr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/whitemarblegranite.com\/tr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/whitemarblegranite.com\/tr\/wp-json\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/whitemarblegranite.com\/tr\/wp-json\/wp\/v2\/comments?post=10909"}],"version-history":[{"count":0,"href":"https:\/\/whitemarblegranite.com\/tr\/wp-json\/wp\/v2\/posts\/10909\/revisions"}],"wp:attachment":[{"href":"https:\/\/whitemarblegranite.com\/tr\/wp-json\/wp\/v2\/media?parent=10909"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/whitemarblegranite.com\/tr\/wp-json\/wp\/v2\/categories?post=10909"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/whitemarblegranite.com\/tr\/wp-json\/wp\/v2\/tags?post=10909"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}