{"id":20154,"date":"2016-03-25T00:40:14","date_gmt":"2016-03-24T22:40:14","guid":{"rendered":"http:\/\/karasugranite.com\/de\/granit-nedir\/-old"},"modified":"2023-03-11T14:43:00","modified_gmt":"2023-03-11T11:43:00","slug":"granit-nedir-before-import","status":"publish","type":"page","link":"https:\/\/karasugranite.com\/de\/granit-nedir-before-import\/","title":{"rendered":"Granit Nedir?"},"content":{"rendered":"

Granit Nedir ?<\/h1>\n
\n

Granit, sert, kristal yap\u0131l\u0131 minerallerden meydana gelen taneli g\u00f6r\u00fcn\u00fc\u015fl\u00fc magmatik derinlik k\u00fcltesi. Pl\u00fcton i\u00e7indeki taneler \u00e7o\u011funlukla g\u00f6zle g\u00f6r\u00fclebilir b\u00fcy\u00fckl\u00fcktedir. Esas mineralleri feldspat\u0131n ortoklas cinsi ile az miktarda plajioklas ve kuvarst\u0131r. Ayr\u0131ca mika, hornblend, piroksen ve ikinci gruba giren turmalin, apatit, zirkon, grena, manyetit gibi mineraller de bulunabilir.<\/p>\n

Granitlerin renkleri, genellikle a\u00e7\u0131k olmakla birlikte, i\u00e7indeki feldispatlar\u0131n ve di\u011fer minerallerin cins ve miktar\u0131na g\u00f6re gri, pembe, turuncu olabilir.<\/p>\n

Granitler, yery\u00fcz\u00fcnde \u00e7ok yayg\u0131n olarak bulunurlar. \u00c7e\u015fitli yer kabu\u011fu modellerinde g\u00f6r\u00fcn\u00fcr. Yery\u00fcz\u00fcn\u00fcn temelini te\u015fekk\u00fcl ettirdi\u011fi kabul edilmektedir. Do\u011fada dayk, silis ve batolitler halinde bulunabilir.<\/p>\n

Yollarda parke ve bord\u00fcr ta\u015f\u0131, yap\u0131larda yap\u0131 ta\u015f\u0131 olarak \u00e7ok eskiden beri bol miktarda kullan\u0131lmaktad\u0131r. A\u015f\u0131nmaya, bas\u0131nca, darbeye kar\u015f\u0131 dayan\u0131kl\u0131, g\u00fczel renkli ve iyi cila kabul eder. Atmosfer tesirlerine ve ayr\u0131\u015fmaya kar\u015f\u0131 direnci y\u00fcksektir. G\u00fcn\u00fcm\u00fczde daha \u00e7ok parke ve bord\u00fcr ta\u015f\u0131 ve baz\u0131 b\u00fcy\u00fck yap\u0131larda kaplama ta\u015f\u0131 olarak kullan\u0131lmaktad\u0131r.<\/p>\n

Granit, yeri\u00e7inde 400 santigrat derece civar\u0131nda bir \u0131s\u0131ya sahip olup, so\u011fumas\u0131 birka\u00e7 bin y\u0131l gibi \u00e7ok uzun bir zaman\u0131 kapsar. Bu \u0131s\u0131 ayn\u0131 zamanda jeotermal sular\u0131n da kayna\u011f\u0131d\u0131r. Yeri\u00e7ine s\u00fcz\u00fclen sular\u0131n, granitlerin \u00e7atlaklar\u0131 aras\u0131ndaki hareketi, hem granitin y\u00fcksek \u0131s\u0131s\u0131 ile su s\u0131cakl\u0131\u011f\u0131n\u0131 artt\u0131r\u0131r hem de \u00e7\u00f6z\u00fcnebilir haldeki mineraller suyun b\u00fcnyesine dahil olur. Jeotermal sular\u0131n olu\u015fumu bu \u015fekilde ger\u00e7ekle\u015fir.<\/p>\n

Bile\u015fimi ve bulunu\u015fu<\/h1>\n
\n

Granitlerde kuvars, genellikle hacmen % 20’nin \u00fczerindedir. Derinlik k\u00fclteleri aras\u0131nda hacmen % 40’tan fazla kuvars ihtiva eden t\u00fcre rastlanmaz. Kuvars ve a\u011f\u0131r silikatlar bak\u0131m\u0131ndan zengin olan kaya\u00e7lar gabro s\u0131n\u0131f\u0131na girer. Esas bile\u015feni olan feldspat plajioklas ve ortoklas (alkali feldspat) halinde olmas\u0131 m\u00fcmk\u00fcnd\u00fcr. Birinin di\u011ferine oran\u0131 genellikle ikiden azd\u0131r. Granitlerde bulunan ikinci ana mineraller muskovit, biyotit, amfibol, piroksen veya nadiren fayalit (demirli olivin) olarak s\u0131ralanabilir. Genellikle bunlardan iki veya \u00fc\u00e7\u00fc bir arada bulunur.\u00c7e\u015fitli s\u0131n\u0131flamalarda koyu renkli minerallerin oran\u0131 farkl\u0131 olmakla birlikte hacmen % 20’den fazla koyu renkli mineral ihtiva eden ta\u015flara genellikle granit ad\u0131 verilmemektedir.<\/p>\n

Olu\u015fum teorileri<\/h1>\n
\n

Ba\u015fl\u0131ca iki z\u0131t g\u00f6r\u00fc\u015f vard\u0131r;
\nMa\u011fmatik: Granitlerin, ana s\u0131v\u0131n\u0131n veya s\u0131v\u0131 kristalin, kristalle\u015fmesi sonucu olu\u015ftu\u011funu kabul eder.
\nTransformist: Granitlerin ma\u011fma olmaks\u0131z\u0131n meydana geldi\u011fini ileri s\u00fcrer. Granitlerin tortul k\u00fcltelerin \u00e7o\u011funlukla kat\u0131 halde metamorfizma sonucu ortaya \u00e7\u0131kt\u0131\u011f\u0131 g\u00f6r\u00fc\u015f\u00fcndedir.<\/p>\n","protected":false},"excerpt":{"rendered":"

Granit Nedir ? Granit, sert, kristal yap\u0131l\u0131 minerallerden meydana gelen taneli g\u00f6r\u00fcn\u00fc\u015fl\u00fc magmatik derinlik k\u00fcltesi….<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-20154","page","type-page","status-publish","hentry"],"translation":{"provider":"WPGlobus","version":"3.0.0","language":"de","enabled_languages":["tr","en","de"],"languages":{"tr":{"title":true,"content":true,"excerpt":false},"en":{"title":false,"content":false,"excerpt":false},"de":{"title":false,"content":false,"excerpt":false}}},"_links":{"self":[{"href":"https:\/\/karasugranite.com\/de\/wp-json\/wp\/v2\/pages\/20154","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/karasugranite.com\/de\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/karasugranite.com\/de\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/karasugranite.com\/de\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/karasugranite.com\/de\/wp-json\/wp\/v2\/comments?post=20154"}],"version-history":[{"count":11,"href":"https:\/\/karasugranite.com\/de\/wp-json\/wp\/v2\/pages\/20154\/revisions"}],"predecessor-version":[{"id":21130,"href":"https:\/\/karasugranite.com\/de\/wp-json\/wp\/v2\/pages\/20154\/revisions\/21130"}],"wp:attachment":[{"href":"https:\/\/karasugranite.com\/de\/wp-json\/wp\/v2\/media?parent=20154"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}