{"id":13850,"date":"2021-07-26T16:40:40","date_gmt":"2021-07-26T13:40:40","guid":{"rendered":"https:\/\/www.maden.net\/taslarin-dunyasi\/"},"modified":"2021-07-26T16:40:40","modified_gmt":"2021-07-26T13:40:40","slug":"taslarin-dunyasi","status":"publish","type":"post","link":"https:\/\/www.maden.net\/ar\/taslarin-dunyasi\/","title":{"rendered":"Ta\u015flar\u0131n D\u00fcnyas\u0131"},"content":{"rendered":"

G\u00fcne\u015f etraf\u0131nda d\u00f6nen 9 gezegenden biri olan d\u00fcnyam\u0131z\u0131n 4,6 milyar ya\u015f\u0131nda oldu\u011fu tahmin edilmektedir. Bunun son 50.000 y\u0131ll\u0131k b\u00f6l\u00fcm\u00fcnde insanlar yery\u00fcz\u00fcnde ya\u015famaktad\u0131r.<\/p>\n

KAYA\u00c7LAR<\/h5>\n

G\u00fcne\u015f etraf\u0131nda d\u00f6nen 9 gezegenden biri olan d\u00fcnyam\u0131z\u0131n 4,6 milyar ya\u015f\u0131nda oldu\u011fu tahmin edilmektedir. Bunun son 50.000 y\u0131ll\u0131k b\u00f6l\u00fcm\u00fcnde insanlar yery\u00fcz\u00fcnde ya\u015famaktad\u0131r. Ve insanlar ya\u015fad\u0131klar\u0131 s\u00fcre boyunca, en ilkel insandan bug\u00fcnk\u00fc modern topluma kadar, ta\u015flarla i\u00e7i\u00e7e olmu\u015flard\u0131r. Ta\u015flardaki oyuklardan olu\u015fan ilk evlerinden, yani ma\u011faralardan, bug\u00fcnk\u00fc modern g\u00f6kdelenlere kadar evlerini hep ta\u015flarla in\u015fa etmi\u015flerdir. El aletlerinde, mutfak e\u015fyalar\u0131nda, dekoratif ama\u00e7la ta\u015flar\u0131 kullanm\u0131\u015f, hatta ta\u015flar\u0131, s\u00fcslenme ama\u00e7l\u0131 olarak tak\u0131 \u015feklinde v\u00fccutlar\u0131nda ta\u015f\u0131m\u0131\u015flard\u0131r. Tarih \u00e7a\u011flar\u0131 bile ta\u015flar\u0131n kullan\u0131m\u0131na g\u00f6re isimlendirilmi\u015ftir. (Yontma ta\u015f devri, cilal\u0131 ta\u015f devri)<\/p>\n

Bug\u00fcn de dekoratif veya i\u015flevsel alanlarda kullan\u0131lmas\u0131n\u0131n yan\u0131 s\u0131ra in\u015faat, madencilik ve altyap\u0131 sekt\u00f6rlerinde ana hammaddelerden biri olarak ta\u015flar insanlar taraf\u0131ndan kullan\u0131lmaya devam etmektedir. Hayat\u0131m\u0131zda bu kadar \u00f6nemli bir yere sahip olan ta\u015flar\u0131, yani genel ismiyle kaya\u00e7lar\u0131 daha yak\u0131ndan inceleyecek olursak;<\/p>\n

Gezegenimizin, yery\u00fcz\u00fcnden yakla\u015f\u0131k 16km derinli\u011fe kadar olan k\u0131sm\u0131na yerkabu\u011fu ismi verilir ve yerkabu\u011funun %75’i yaln\u0131zca 2 elementten olu\u015fmaktad\u0131r (Oksijen %46,6 ve Silis %27,7). Yerkabu\u011funun %99’u ise 8 elementten meydana gelmektedir (Oksijen ve silise ilave olarak Aluminyum %8,1, Demir %5, Kalsiyum %3,6, Sodyum %2,8, Potasyum %2,6, Magnezyum %2,1 ve di\u011fer elementler %1,5). Bu elementler bir araya gelerek kaya\u00e7lar\u0131n yap\u0131ta\u015flar\u0131 olan mineralleri olu\u015fturur. Yery\u00fcz\u00fcnde yakla\u015f\u0131k 2.000 farkl\u0131 do\u011fal mineral vard\u0131r. Ancak bunlar\u0131n yaln\u0131zca 10 tanesi kaya\u00e7lar\u0131n olu\u015fumunda \u00f6nem sahibidir.<\/p>\n

Kaya\u00e7lar bir veya birden fazla mineralin bir araya gelmesiyle olu\u015fan kat\u0131 birikintilerdir. Temel olarak 3 ana kaya\u00e7 t\u00fcr\u00fc vard\u0131r. Magmatik Kaya\u00e7lar, Sedimanter (Tortul veya \u00e7\u00f6kel) Kaya\u00e7lar ve Metamorfik (Ba\u015fkala\u015f\u0131m) Kaya\u00e7lar. Yery\u00fcz\u00fcndeki kaya\u00e7lar\u0131n %95’i magmatik kaya\u00e7, %1’i sedimanter kaya\u00e7 ve %4’\u00fc ba\u015fkala\u015f\u0131m kaya\u00e7lard\u0131r.<\/p>\n

MAGMAT\u0130K KAYA\u00c7LAR<\/h5>\n

\"\"Erimi\u015f durumda bir silikat hamuru olan magman\u0131n, yery\u00fcz\u00fcnde veya y\u00fczeyden daha derinlerde so\u011fumas\u0131 ve kat\u0131la\u015fmas\u0131 ile meydana gelmi\u015f kaya\u00e7 t\u00fcr\u00fcd\u00fcr. Magmatik kaya\u00e7lar genel karakteristik olarak kristallerden olu\u015fmu\u015f k\u00fctleler halindedir. Magmatik kaya\u00e7lar\u0131n 2 t\u00fcr\u00fc vard\u0131r:<\/p>\n

Obsidyen: Lavlar\u0131n \u00e7ok h\u0131zl\u0131 so\u011fumas\u0131 sonucu olu\u015fan bir volkanik cam t\u00fcrevidir. Obsidyen tipik bir \u00f6zelli\u011fi olan keskin kenarlar\u0131 ve sert yap\u0131s\u0131 nedeniyle ilkel insanlar taraf\u0131ndan kesici alet olarak kullan\u0131lm\u0131\u015ft\u0131r.<\/em><\/p>\n

 <\/p>\n

1. Pl\u00fctonik (Sokulum veya derinlik) kaya\u00e7lar<\/strong><\/p>\n

Y\u00fckselen magman\u0131n yery\u00fcz\u00fcne eri\u015femeden, herhangi bir derinlikte so\u011fuyarak kat\u0131la\u015fmas\u0131 sonucu olu\u015fur. Bu kaya\u00e7lar, \u00fczerlerindeki kaya\u00e7 tabakalar\u0131 a\u015f\u0131nd\u0131\u011f\u0131nda yery\u00fcz\u00fcne ula\u015f\u0131r. Magma derin tabakalarda yava\u015f yava\u015f so\u011fudu\u011fundan bu kaya\u00e7larda tam kristalle\u015fme olur. En \u00e7ok rastlanan pl\u00fctonik kaya\u00e7 granittir. Ayr\u0131ca diyonit, siyenit ve gabro da pl\u00fctonik kaya\u00e7lara verilebilecek \u00f6rneklerdir. \u00a0Pl\u00fctonik kaya\u00e7lar genellikle magman\u0131n yava\u015f so\u011fumas\u0131 nedeniyle olu\u015fan iri kristaller i\u00e7erir ve kaba taneli bir yap\u0131ya sahiptir.<\/p>\n

\"\" \"\"<\/p>\n

Granit: En s\u0131k rastlanan sokulum kayac\u0131 granittir. Granit temelde iri kuvars , mika ve feldspattan meydana gelir. Genellikle benekli bir g\u00f6r\u00fcn\u00fcme sahiptir. B\u00fcnyesinde bulunan minerallerin oranlar\u0131ndaki de\u011fi\u015fimlere g\u00f6re griden k\u0131rm\u0131z\u0131ya de\u011fi\u015fen renklere sahiptir.<\/em><\/p>\n

2. Volkanik (P\u00fcsk\u00fcr\u00fck) Kaya\u00e7lar<\/strong><\/p>\n

Volkanik kaya\u00e7lar magman\u0131n bir volkandan lav olarak p\u00fcsk\u00fcrmesi ile yery\u00fcz\u00fcne ula\u015fmas\u0131 ve orada so\u011fuyarak kat\u0131la\u015fmas\u0131 sonucu olu\u015fur. Magma yery\u00fcz\u00fcne \u00e7\u0131kt\u0131\u011f\u0131nda daha h\u0131zl\u0131 so\u011fudu\u011fundan bu kaya\u00e7lar kristal olmayan, cams\u0131 bir hamurdan olu\u015fur. Bu kaya\u00e7lar ince taneli veya cams\u0131 g\u00f6r\u00fcn\u00fcml\u00fc olur. En s\u0131k rastlanan volkanik kaya\u00e7 bazaltt\u0131r. Ayr\u0131ca andezit, obsidiyen ve t\u00fcf de volkanik kaya\u00e7lara verilebilecek \u00f6rneklerdendir.<\/p>\n

\"\"<\/p>\n

Bazalt: En s\u0131k rastlanan p\u00fcsk\u00fcr\u00fck kaya\u00e7 t\u00fcr\u00fc olan bazalt kat\u0131la\u015fm\u0131\u015f lavdan olu\u015fur. Olduk\u00e7a sert bir yap\u0131s\u0131 vard\u0131r.<\/em><\/p>\n

\"\"<\/p>\n

Obsidyen: Lavlar\u0131n \u00e7ok h\u0131zl\u0131 so\u011fumas\u0131 sonucu olu\u015fan bir volkanik cam t\u00fcrevidir. Obsidyen tipik bir \u00f6zelli\u011fi olan keskin kenarlar\u0131 ve sert yap\u0131s\u0131 nedeniyle ilkel insanlar taraf\u0131ndan kesici alet olarak kullan\u0131lm\u0131\u015ft\u0131r.<\/em><\/p>\n

SED\u0130MANTER KAYA\u00c7LAR<\/h5>\n

\"\"B\u00fcy\u00fck Kanyon: Amerika’da bulunan B\u00fcy\u00fck Kanyon, sedimanter kaya\u00e7lara \u00e7ok g\u00fczel bir \u00f6rnek te\u015fkil eder. Kire\u00e7 ta\u015flar\u0131 ve k\u0131rm\u0131z\u0131 kumta\u015flar\u0131n\u0131n a\u015f\u0131nmas\u0131 ile olu\u015fmu\u015ftur.<\/em><\/p>\n

Sedimanter kaya\u00e7lar ayn\u0131 zamanda tortul kaya\u00e7lar veya \u00e7\u00f6kel kaya\u00e7lar olarak da bilinir. \u0130simlerinden de anla\u015f\u0131laca\u011f\u0131 gibi bu t\u00fcr kaya\u00e7lar, maddelerin \u00e7\u00f6kmesi (tortula\u015fmas\u0131) sonucu meydana gelirler.\u00a0 Varolan kaya\u00e7lar, akarsular, r\u00fczgar, g\u00fcne\u015f, dalgalar gibi d\u0131\u015f etkenler taraf\u0131ndan veya kimyasal yollarla ayr\u0131\u015ft\u0131r\u0131l\u0131r, a\u015f\u0131nd\u0131r\u0131l\u0131r ve k\u00fc\u00e7\u00fck kaya\u00e7 par\u00e7ac\u0131klar\u0131 ve mineraller halinde d\u00f6k\u00fcl\u00fcr. \u00c7\u00f6kel olarak isimlendirilen bu d\u00f6k\u00fcnt\u00fcler er ge\u00e7 yeni bir yere ta\u015f\u0131n\u0131r. Genellikle akarsu yataklar\u0131na veya denize ta\u015f\u0131nan bu \u00e7\u00f6keller katmanlar halinde birikir. \u00a0Bu \u00e7\u00f6keller y\u0131\u011f\u0131lan maddelerin a\u011f\u0131rl\u0131\u011f\u0131 alt\u0131nda s\u0131k\u0131\u015f\u0131rlar, hacimleri k\u00fc\u00e7\u00fcl\u00fcr, g\u00f6zenekleri azal\u0131r ve i\u00e7erdikleri su d\u0131\u015far\u0131 at\u0131l\u0131r. Kendi i\u00e7lerinde meydana gelen kimyasal tepkimelerle mineraller olu\u015fur. Bu mineraller ve \u00e7\u00f6kelin i\u00e7ine kar\u0131\u015fan di\u011fer organik maddeler bir \u00e7imento vazifesi g\u00f6r\u00fcr ve \u00e7\u00f6keller zaman i\u00e7inde sertle\u015ferek ta\u015fla\u015f\u0131r. Y\u00fczbinlerce hatta milyonlarca y\u0131ll\u0131k bu s\u00fcre\u00e7 sonunda sedimanter kaya\u00e7lar olu\u015fur. Kaya\u00e7lar\u0131n yery\u00fcz\u00fcnde g\u00f6r\u00fcnd\u00fc\u011f\u00fc yama\u00e7larda, tortul katmanlar\u0131n\u0131 \u00e7\u0131plak g\u00f6zle g\u00f6rmek m\u00fcmk\u00fcnd\u00fcr. Sedimanter kaya\u00e7lar, kimyasal, organik ve fiziksel olmak \u00fczere \u00fc\u00e7e ayr\u0131l\u0131r.<\/p>\n

\"\"<\/p>\n

Kalker: En yayg\u0131n olarak bilinen tortul kaya\u00e7 kalkerdir (Kire\u00e7 ta\u015f\u0131). Kalsiyum karbonat i\u00e7erir. Kire\u00e7 \u00fcretiminde kullan\u0131l\u0131r. Minimum %90 oran\u0131nda kalsiyum karbonat i\u00e7eren kaya\u00e7lara kalker denir. Kalker \u00e7imento yap\u0131m\u0131nda kullan\u0131l\u0131r.<\/em><\/p>\n

1. Kimyasal sedimanter kaya\u00e7lar<\/strong><\/p>\n

Baz\u0131 sedimanter kaya\u00e7lar tuzlu sular\u0131n buharla\u015fmas\u0131 ve doygun eriyiklerin \u00e7\u00f6kelmesi sonucu olu\u015fur. En yayg\u0131n bilinen kimyasal tortul kaya\u00e7 kire\u00e7 ta\u015f\u0131d\u0131r. Jips (al\u00e7\u0131ta\u015f\u0131) ve halit (kaya tuzu) bu kaya\u00e7lara \u00f6rnek olarak verilebilir. Ayr\u0131ca g\u00f6l kenarlar\u0131ndaki tuz birikintileri, su kaynaklar\u0131 \u00e7evresindeki ta\u015fla\u015fmalar da kimyasal sedimanter kaya\u00e7 t\u00fcrleridir.<\/p>\n

\"\"<\/p>\n

Jips: Al\u00e7\u0131 \u00fcretiminde kullan\u0131lan jips, al\u00e7\u0131ta\u015f\u0131 olarak da bilinir. Al\u00e7\u0131ta\u015f\u0131 ve kayatuzu genellikle deniz suyunun buharla\u015ft\u0131\u011f\u0131 eski deniz yataklar\u0131nda bulunur.<\/em><\/p>\n

2. Fiziksel sedimanter kaya\u00e7lar<\/strong><\/p>\n

Mineral ve ta\u015f par\u00e7alar\u0131n\u0131n denizde veya karada bulunan \u00e7\u00f6kelme havzalar\u0131nda birikerek ta\u015fla\u015fmas\u0131 sonucu olu\u015fmu\u015f kaya\u00e7lard\u0131r. Kumta\u015f\u0131, kilta\u015f\u0131, konglomera (\u00e7ak\u0131l ta\u015f\u0131) bu t\u00fcr kaya\u00e7lara verilebilecek \u00f6rneklerdendir.<\/p>\n

\"\"<\/p>\n

Konglomera: Bu kaya\u00e7taki \u00e7ak\u0131llar, deniz veya akarsular\u0131n taban\u0131nda hareket ettirilirken yuvarlakla\u015fm\u0131\u015ft\u0131r. Daha sonra kademeli olarak birbirlerine yap\u0131\u015farak konglomera ad\u0131 verilen bu kayac\u0131 olu\u015fturmu\u015flard\u0131r.<\/em><\/p>\n

,\"\"<\/p>\n

Kumta\u015f\u0131: Kumta\u015f\u0131 ince kum tanelerinin biraraya gelmesinden olu\u015fur. Kuvars tanelerinin r\u00fczgar taraf\u0131ndan yuvarlakla\u015ft\u0131r\u0131ld\u0131\u011f\u0131 ve parlat\u0131ld\u0131\u011f\u0131 \u00e7\u00f6l ortam\u0131nda olu\u015fan kumta\u015flar\u0131 k\u0131rm\u0131z\u0131 renkli olur.\u00a0<\/em><\/p>\n

3. Organik sedimanter kaya\u00e7lar<\/strong><\/p>\n

S\u00fcngerler, mercanlar, algler gibi kabuklu organizmalar\u0131n veya bitki kal\u0131nt\u0131lar\u0131n\u0131n ta\u015fla\u015farak fosil haline gelmesinden olu\u015fan kaya\u00e7lard\u0131r. Ta\u015fk\u00f6m\u00fcr\u00fc, linyit, mercan kayalar\u0131 ve tebe\u015fir organik tortul kaya\u00e7lardand\u0131r.<\/p>\n

\"\"<\/p>\n

Antrasit: En kaliteli k\u00f6m\u00fcr antrasittir. Antrasit di\u011fer k\u00f6m\u00fcrlerden \u00e7ok daha serttir ve dokunuldu\u011funda eli boyamaz. Di\u011fer b\u00fct\u00fcn k\u00f6m\u00fcrlerden daha fazla karbon i\u00e7erir. Bu nedenle az duman \u00e7\u0131kar\u0131r, \u00e7ok \u0131s\u0131 verir ve k\u00f6m\u00fcrlerin en de\u011ferlisidir.<\/em><\/p>\n

METAMORF\u0130K (BA\u015eKALA\u015eIM) KAYA\u00c7LAR<\/h5>\n

Metamorfik kaya\u00e7lar, daha \u00f6nce anlat\u0131lan magmatik veya sedimanter kaya\u00e7lar\u0131n \u0131s\u0131 ve bas\u0131n\u00e7 etkisiyle ba\u015fkala\u015fmas\u0131 sonucu meydana gelmi\u015f kaya\u00e7lard\u0131r. Yeralt\u0131nda kalan kaya\u00e7lar, da\u011f olu\u015fumu s\u00fcre\u00e7lerinde magman\u0131n yery\u00fcz\u00fcne \u00e7\u0131kmak i\u00e7in \u00fcst tabakalar\u0131 zorlamas\u0131 esnas\u0131nda, s\u0131cak bir magmatik k\u00fctle etraf\u0131nda y\u00fcksek s\u0131cakl\u0131klar\u0131n etkisi alt\u0131nda kalabilir ve s\u0131k\u0131\u015fabilir. Kalkerden mermer, k\u00f6m\u00fcrden elmas, kilta\u015f\u0131ndan \u015fist olu\u015fumlar\u0131 bu ba\u015fkala\u015f\u0131mlara \u00f6rnek olarak verilebilir.<\/p>\n

\"\" \"\"<\/p>\n

Mermer: Mermer asl\u0131nda ba\u015fkala\u015f\u0131ma u\u011fram\u0131\u015f bir kire\u00e7 ta\u015f\u0131d\u0131r. Ancak mermer terimi ta\u015f end\u00fcstrisinde di\u011fer kaya\u00e7 \u00e7e\u015fitleri i\u00e7in s\u0131kl\u0131kla kullan\u0131l\u0131r. Mermer \u00e7ekici dokusu, kolay kesilmesi ve parlat\u0131lmas\u0131 sebebiyle dekoratif ama\u00e7la \u00e7ok s\u0131k kullan\u0131l\u0131r.<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"

G\u00fcne\u015f etraf\u0131nda d\u00f6nen 9 gezegenden biri olan d\u00fcnyam\u0131z\u0131n 4,6 milyar ya\u015f\u0131nda oldu\u011fu tahmin edilmektedir. Bunun son 50.000 y\u0131ll\u0131k b\u00f6l\u00fcm\u00fcnde insanlar yery\u00fcz\u00fcnde ya\u015famaktad\u0131r. KAYA\u00c7LAR G\u00fcne\u015f etraf\u0131nda d\u00f6nen 9 gezegenden biri olan d\u00fcnyam\u0131z\u0131n 4,6 milyar ya\u015f\u0131nda oldu\u011fu tahmin edilmektedir. Bunun son 50.000 y\u0131ll\u0131k b\u00f6l\u00fcm\u00fcnde insanlar yery\u00fcz\u00fcnde ya\u015famaktad\u0131r. Ve insanlar ya\u015fad\u0131klar\u0131 s\u00fcre boyunca, en ilkel insandan bug\u00fcnk\u00fc modern…<\/p>\n","protected":false},"author":1,"featured_media":10683,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1,18],"tags":[],"class_list":["post-13850","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-haberler","category-haberler-ar"],"yoast_head":"\nTa\u015flar\u0131n D\u00fcnyas\u0131 - Maden Crushing & Screening<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.maden.net\/ar\/taslarin-dunyasi\/\" \/>\n<meta property=\"og:locale\" content=\"ar_AR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Ta\u015flar\u0131n D\u00fcnyas\u0131 - Maden Crushing & Screening\" \/>\n<meta property=\"og:description\" content=\"G\u00fcne\u015f etraf\u0131nda d\u00f6nen 9 gezegenden biri olan d\u00fcnyam\u0131z\u0131n 4,6 milyar ya\u015f\u0131nda oldu\u011fu tahmin edilmektedir. Bunun son 50.000 y\u0131ll\u0131k b\u00f6l\u00fcm\u00fcnde insanlar yery\u00fcz\u00fcnde ya\u015famaktad\u0131r. KAYA\u00c7LAR G\u00fcne\u015f etraf\u0131nda d\u00f6nen 9 gezegenden biri olan d\u00fcnyam\u0131z\u0131n 4,6 milyar ya\u015f\u0131nda oldu\u011fu tahmin edilmektedir. Bunun son 50.000 y\u0131ll\u0131k b\u00f6l\u00fcm\u00fcnde insanlar yery\u00fcz\u00fcnde ya\u015famaktad\u0131r. 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