首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Geology and isotope geochemistry (C-O-S) of the Diyadin gold deposit, Eastern Turkey: A newly-discovered Carlin-like deposit
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Geology and isotope geochemistry (C-O-S) of the Diyadin gold deposit, Eastern Turkey: A newly-discovered Carlin-like deposit

机译:地质和同位素地球化学(C-O-S)Diyadin金矿,土耳其东部:新发现Carlin-like存款

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摘要

Diyadin mineralization is the first reported gold deposit located in a aillibion.il tectonic environment in Eastern Anatolia. The mineralization is related to N-S and N10-20 deg W-trending fault systems and hosted within the Paleozoic metamorphic basement rocks of the Anatolide-Toride niicrocontinenr. Calc-schist, dolomitic marble and Miocene and Quaternary volcanic rocks comprise the exposed units in the mineralized area. Geochemical signatures, alteration types and host rock characteristics of the Diyadin gold deposit resemble those of Carlin-type deposits. Mineralization is constrained by alteration of overlying volcanic rocks to younger than -14 Ma (K-Ar).
机译:Diyadin矿化是第一个报道黄金矿床位于aillibion。在安纳托利亚东部环境。矿化n和N10-20度有关W-trending断层系统和内举办古生代变质基底岩石的Anatolide-Toride niicrocontinenr .白云质大理岩和中新世和第四纪火山岩组成单位矿化区。蚀变类型和母岩特征Diyadin黄金矿床相似Carlin-type存款。受到上覆火山的变更岩石小于-14 Ma (K-Ar)。

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