{"id":282,"date":"2024-02-28T11:46:34","date_gmt":"2024-02-28T08:46:34","guid":{"rendered":"https:\/\/www.pirlantaakademi.com\/blog\/?p=282"},"modified":"2024-04-17T11:10:46","modified_gmt":"2024-04-17T08:10:46","slug":"elmaslar-nasil-olusmustur","status":"publish","type":"post","link":"https:\/\/www.pirlantaakademi.com\/blog\/elmaslar-nasil-olusmustur\/","title":{"rendered":"Elmaslar Nas\u0131l Olu\u015fmu\u015ftur?"},"content":{"rendered":"\n

Elmas, yery\u00fcz\u00fcnde bulunan en sert ve bile\u015fimi en basit olan de\u011ferli ta\u015ft\u0131r.<\/p>\n\n\n\n

Elmaslar\u0131n olu\u015fmas\u0131na olanak sa\u011flayan ko\u015fullar, gezegenimizde milyonlarca y\u0131ld\u0131r bulunmuyor.<\/p>\n\n\n\n

Yerk\u00fcrenin olu\u015fmaya ba\u015flad\u0131\u011f\u0131 erken d\u00f6nemlerde kat\u0131 madde yo\u011funla\u015f\u0131p bir k\u00fcreye d\u00f6n\u00fc\u015ft\u00fck\u00e7e, gezegenin merkezi de \u00e7ok y\u00fcksek s\u0131cakl\u0131k ve bas\u0131n\u00e7 alt\u0131nda kalm\u0131\u015ft\u0131r. Derin tabakalardaki bu ko\u015fullar saf karbon \u00e7\u00f6keltilerinin kristalle\u015ferek elmasa d\u00f6n\u00fc\u015fmesine neden olmu\u015ftur. Bir elmas saf karbon i\u00e7erir ve karbon tozu ile elmas aras\u0131nda kimyasal bir farkl\u0131l\u0131k olmasa da, aralar\u0131ndaki fiziksel farkl\u0131l\u0131k hem \u00e7ok b\u00fcy\u00fck, hem de hayret vericidir.<\/p>\n\n\n\n

Yerk\u00fcrenin d\u0131\u015f katmanlar\u0131 so\u011fuduk\u00e7a, bas\u0131n\u00e7lar artm\u0131\u015f ve kat\u0131 kaya tabakalar\u0131 yerlerinden oynayarak yar\u0131lm\u0131\u015ft\u0131r. S\u0131v\u0131 k\u00fctle (magma) ak\u0131nt\u0131lar\u0131 ise volkanik patlamalar ile y\u00fczeye \u00e7\u0131kmak zorunda kalm\u0131\u015f ve bu maddenin bir k\u0131sm\u0131 yerk\u00fcrenin derinliklerinde olu\u015fmaya ba\u015flayan elmas kristallerini de kendisi ile birlikte y\u00fczeye ta\u015f\u0131m\u0131\u015ft\u0131r.<\/p>\n\n\n\n

Yerk\u00fcrenin y\u00fczeyi so\u011fuduk\u00e7a, elmas cevheri ta\u015f\u0131yan k\u00fctleler kat\u0131la\u015fmakta ve bug\u00fcn elmaslar bu k\u00fctlelerin i\u00e7inden \u00e7\u0131kar\u0131lmaktad\u0131r.<\/p>\n\n\n\n

\"\"<\/figure>\n\n\n\n

Elmaslar, milyarlarca y\u0131l \u00f6nce yerk\u00fcrenin derinliklerinde, karbonun korkun\u00e7 bir s\u0131cakl\u0131k ve bas\u0131n\u00e7 alt\u0131nda kristalle\u015fmeye ba\u015flamas\u0131 ile olu\u015ftu. Elmas cevheri i\u00e7eren magma, volkanik patlamalar\u0131n sonucunda y\u00fczeye \u00e7\u0131kt\u0131. Daha sonra volkanik hareket yat\u0131\u015f\u0131p so\u011fuduk\u00e7a, elmaslar “mavi tabaka” ya da “kimberlit” ad\u0131 verilen kat\u0131la\u015fm\u0131\u015f magman\u0131n i\u00e7inde kald\u0131lar. Kimberlit damarlar\u0131ndan al\u00fcvyon yataklar\u0131na kadar bir\u00e7ok de\u011fi\u015fik t\u00fcrde elmas madencili\u011fi vard\u0131r.<\/p>\n\n\n\n

\"\"<\/figure>\n\n\n\n

Y\u00fczy\u0131llar boyunca kimberlit damarlar\u0131ndaki a\u015f\u0131nma, elmaslar\u0131 \u00f6nce ya\u011fmur suyu, sonra da \u0131rmaklarla ta\u015f\u0131yarak, ikincil b\u00f6lgelere getirmi\u015f ve al\u00fcvyon tabakalar\u0131 olu\u015fturmu\u015ftur.<\/p>\n","protected":false},"excerpt":{"rendered":"

Elmas, yery\u00fcz\u00fcnde bulunan en sert ve bile\u015fimi en basit olan de\u011ferli ta\u015ft\u0131r. Elmaslar\u0131n olu\u015fmas\u0131na olanak sa\u011flayan ko\u015fullar, gezegenimizde milyonlarca y\u0131ld\u0131r bulunmuyor. Yerk\u00fcrenin olu\u015fmaya ba\u015flad\u0131\u011f\u0131 erken d\u00f6nemlerde kat\u0131 madde yo\u011funla\u015f\u0131p bir k\u00fcreye d\u00f6n\u00fc\u015ft\u00fck\u00e7e, gezegenin merkezi de \u00e7ok y\u00fcksek s\u0131cakl\u0131k ve bas\u0131n\u00e7 alt\u0131nda kalm\u0131\u015ft\u0131r. Derin tabakalardaki bu ko\u015fullar saf karbon \u00e7\u00f6keltilerinin kristalle\u015ferek elmasa d\u00f6n\u00fc\u015fmesine neden olmu\u015ftur. Bir … <\/p>\n

Okumaya devam et “Elmaslar Nas\u0131l Olu\u015fmu\u015ftur?”<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"_links":{"self":[{"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/posts\/282"}],"collection":[{"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/comments?post=282"}],"version-history":[{"count":1,"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/posts\/282\/revisions"}],"predecessor-version":[{"id":285,"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/posts\/282\/revisions\/285"}],"wp:attachment":[{"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/media?parent=282"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/categories?post=282"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.pirlantaakademi.com\/blog\/wp-json\/wp\/v2\/tags?post=282"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}