Granit, asidik magmatik kaya\u00e7 i\u00e7inde yer alan m\u00fcdahaleci bir kaya\u00e7t\u0131r. Bu kategorideki en yayg\u0131n kaya t\u00fcr\u00fcd\u00fcr. \u00c7o\u011fu 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. Granitin ana mineralleri kuvars, potas feldispat ve asit plajiyoklazd\u0131r ve ikincil mineraller biyotit, hornblend ve bazen az miktarda piroksendir. Potas feldispat i\u00e7eri\u011fi genellikle plajiyoklaz i\u00e7eri\u011finden daha fazlad\u0131r. \u0130ki i\u00e7erik aras\u0131ndaki ili\u015fki genellikle potas feldispat\u0131n toplam feldispat\u0131n \u00fc\u00e7te ikisini, plajiyoklaz\u0131n \u00fc\u00e7te birini olu\u015fturdu\u011fu ve potas feldispat\u0131n granitte daha fazla oldu\u011fu \u015feklindedir. A\u00e7\u0131k et k\u0131rm\u0131z\u0131s\u0131d\u0131r, ayn\u0131 zamanda gri ve gridir. Kirli beyaz potas feldispat ve plajiyoklaz\u0131 el numunelerinde ay\u0131rt etmek genellikle zordur. \u015eu anda, bu iki feldspat\u0131n \u00e7ift kristal \u00f6zelliklerini dikkatlice g\u00f6zlemlemeliyiz, \u00e7\u00fcnk\u00fc plajiyoklaz\u0131n \u00e7ift kristalleri vard\u0131r. El numunelerini d\u00f6nd\u00fcr\u00fcrken, plajiyoklaz kristalleri \u00fczerinde d\u00fczenli a\u00e7\u0131k ve koyu agregatlar oldu\u011funu g\u00f6rebiliriz. Bu, farkl\u0131 parlakl\u0131k derecelerine sahip kristallerin iki yar\u0131s\u0131 olarak g\u00f6r\u00fcnen bir kaset \u00e7ift kristaldir.<\/p>\n
Granit, koyu renkli minerallerin t\u00fcrlerine g\u00f6re de adland\u0131r\u0131labilir. \u00d6rne\u011fin, koyu mineraller esas olarak biyotittir ve yayg\u0131n bir granit t\u00fcr\u00fc olan biyotit granit olarak adland\u0131r\u0131labilir. Biyotit ve muskovit i\u00e7eri\u011fi e\u015fite yak\u0131nsa, dimika granit olarak adland\u0131r\u0131labilir. Koyu renkli mineral esas olarak hornblend ise hornblend granit olarak adland\u0131r\u0131l\u0131r. Koyu mineral esas olarak piroksen ise piroksen olarak adland\u0131r\u0131l\u0131r. Neredeyse hi\u00e7 koyu mineral i\u00e7ermeyen ta\u015f granit Baigangite olarak adland\u0131r\u0131labilir.<\/p>\n
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Granite is an intrusive rock in acidic magmatic rock. This is the most common type of rock in this category. Most of it is 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 of granite are quartz, […]<\/p>","protected":false},"author":8,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[2343],"tags":[],"class_list":["post-11336","post","type-post","status-publish","format-standard","hentry","category-news"],"acf":[],"_links":{"self":[{"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/posts\/11336","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/users\/8"}],"replies":[{"embeddable":true,"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/comments?post=11336"}],"version-history":[{"count":0,"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/posts\/11336\/revisions"}],"wp:attachment":[{"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/media?parent=11336"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/categories?post=11336"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/mqmarble.com\/tr\/wp-json\/wp\/v2\/tags?post=11336"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}