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- W2885873493 abstract "Alibaltalu laterit yatagi, Bati Azerbaycan bolgesinde (KB Iran), Shahindezh’in yaklasik 20 km KD kesiminde yer almaktadir. Bu yatak, Triyas yasli Elika dolomitleri ve Jura yasli Shemshak kumtaslarinin siniri boyunca tabaka sekilli mercekler halinde olusmustur. Bohmit, diyaspor, kaolinit, muskovit-illit, rutil, anatas, hematit ve gotit mineralleri iceren bu yatak dort farkli cevher fasiyesi ile iliskili olarak gelismis olup bunlar: 1) ferrit, 2) laterit, 3) boksitik kaolinit ve 4) kaolinitik boksit fasiyesleridir. Petrografik olarak cevher ornekleri konglomeratik, yuvarlaklasmis-tanesel, damarcikli, kolloform, pelitomorfik, yalanci porfiritik, noduler ve sungerimsi dokular sergiler. Yatak uzerinde secilmis bazi hatlar uzerindeki Al, Si, Ti, HFSE (yuksek degerliklikatyon elementleri), DNTE (LREE), YNTE (HREE), U, ve Th’un yayilim ozellikleri, gunlenme (weathering) islemleri sirasinda demirlenme-demir yikanmasi olaylarinin onemli bir rol oynadigini gostermistir. Nadir toprak element dagilim desenlerinin kondrite normalize edildigi diyagramlar, bu yatagin olusumu sirasinda ANTE’den (agir nadir toprak elementleri) HNTE (hafif nadir toprak elementleri) ayrimlasmasinin oldukca dusuk oldugunu ve zayif Eu anomalisi olustugunu gostermistir. Bu ozellikler Al2O3/TiO2 oranlari ve gunlenme sirasinda Al’un Fe’den ayrimlasmasi, bu yatagin orijinal kayasinin mafik ozelliklerde olabilecegini isaret etmektedir. Zayif hareketli elementlerin jeokimyasal ozellikleri incelendiginde bu yatagin buyuk olasilikla bazaltik ile andezitik bir ana kayadan gunlenme yoluyla olustugu anlasilmaktadir. Cevherdeki Ni, Cr, Zr ve Gz gibi elementlerin dagilim ozelliklerine bakildiginda bu yatagin oncelikle yerinde zenginlesme ile olustugu, ancak daha sonraki asinim ve tasinim sureclerinde diger kayac parcalari ile karisarak guncel konumuna yeniden cokeldigi anlasilmaktadir." @default.
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- W2885873493 date "2014-06-01" @default.
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- W2885873493 title "GEOCHEMICAL CHARACTERISTICS OF LATERITES: THE AILIBALTALU DEPOSIT, IRAN" @default.
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- W2885873493 doi "https://doi.org/10.19111/bmre.55769" @default.
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