首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Geology, geochemistry and Re-Os geochronology of the Jurassic Zeybek volcanogenic massive sulfide deposit (Central Pontides, Turkey)
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Geology, geochemistry and Re-Os geochronology of the Jurassic Zeybek volcanogenic massive sulfide deposit (Central Pontides, Turkey)

机译:侏罗纪Zeybek波动素大规模硫化硫化物矿床地质,地球化学和重新卫生地质学学(中央Pontice)

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摘要

Located in the north of Anatolia, the Pontide Orogenic Belt hosts Turkey's most important volcanogenic massive sulfide (VMS) deposits. Studies completed in the last ten years have discovered new massive sulfide deposits in the Central Pontide zone. The Zeybek VMS deposit is one of these newly-discovered deposits found in the Central Pontides. This deposit is associated with the Cangaldag Metamorphic Complex occurring as east-west-striking tectonic slices. The Cangaldag Metamorphic Complex is an allochthonous mass of metavolcanic, metavolcanidastic and metaclastic rocks in the form of imbricated tectonic slices. Zeybek massive sulfide deposit is located within metaclastic rocks intercalated with mafic sills or lava flows in this complex.
机译:位于安纳托利亚北部,Pontide Orentenic皮带寄宿土耳其最重要的火山岩大规模硫化物(VMS)沉积物。 在过去十年中完成的研究发现了中央岩石区的新型硫化物沉积物。 Zeybek VMS存款是中央Pontides中发现的这些新发现的矿床之一。 这种沉积物与作为东西醒目的构造切片发生的苍苍变质复合物有关。 CangaldAg变质复合物是一种表征物质的弥补构造切片形式的甲状腺嘧啶,荟萃划分和肉质岩石。 Zeybek大规模硫化物沉积物位于Mafic Sills或熔岩流内插入的Metaclastic岩石内,在这件机中。

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