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Tongling Ore District Massive Sulfide Deposits in Geological Features

机译:铜陵矿区地质特征硫化物矿床

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Pyrite-type massive sulfide deposits widely occur within carboniferous sedimentary-exhalative ore-bearing rocks of the huanglong formation in tongling city of Anhui province. The deposit, characterized by a representative two-layer texture, consists of the exhalation phase massive stratiform ore bed in the upper part and the feeder channelway phase disseminated-stockwork orebody in the lower part. Showing a clear characteristics, Ore has vertical zonal from bottom to top, Zonation rocks have: Siliceous ore,gypsum ore,pyrite ores,pyrite,barite ores, siderite and Chert ore of duricrust. Deposits were formed a unique hydrothermal explosion breccia veins and irregular network interconnected tubular worm, Dendritic, ginger massive pyrite pipeline system, Mineralization in the form of dispersed multi-sheeted mineralization spout. Thickness is usually no more than 100m.
机译:黄铁矿型大型硫化物沉积物广泛发生在铜陵市黄龙形成的石炭系沉积膨胀岩石中。其特征在于代表性的双层纹理的沉积物,包括在上部的呼气相位巨大层状矿床和下部进料器通道相播放 - 图库中间播放矿体。显示出明显的特点,矿石具有从底部到顶部的垂直扎带,区分岩具有:硅质矿石,石膏矿石,黄铁矿矿石,硫铁矿,晶粒矿石,泥石矿和牙耳矿石的杜兰茨。沉积物形成独特的热热爆炸Breccia静脉和不规则网络相互连接的管状蠕虫,树突状,姜巨大的黄铁矿管道系统,以分散的多纸矿化喷口的形式矿化。厚度通常不超过100米。

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