首页> 外文会议>Proceedings of China Gold City - Zhaoyuan International Symposium on Gold Geology and Exploration >Ore-controlling Structure and Metallogenic Regularity of the No. Ⅶ Ore Body in Xiadian Gold Deposit
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Ore-controlling Structure and Metallogenic Regularity of the No. Ⅶ Ore Body in Xiadian Gold Deposit

机译:夏甸金矿Ⅶ矿体控矿构造及成矿规律

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Located to the eastern side of the famous Yishu Fracture Zone, the Xiadian gold deposit is hosted in the Jiaobei Uplift (the third rank tectonic unit) in the Ludong (eastern Shandong) Rise ( the second rank tectonic unit) tectonically. The metamorphic rocks of the Ar-chean Jiaodong Group are found to the southeastern side of the mine and Quaternary sediments are scarcely distributed. Igneous rock in the mine is mainly the Luojiahe biotite granite and is exposed to the northwestern part of the mine. The ore-controlling structures of the mine are mainly featured by faults, and the Zhaoyuan-Pingdu (Zhaoping) Fault Zone runs across the mine. The middle sector of the Zhaoyuan-Pingdu Fault Zone, called the Zhixia-Jiangjiayao Fault and its secondary and associated faults, make up the ore-controlling structures of the mine. From southwest to northeast, the Xiadian gold deposit comprises four ore bodies; No. Ⅰ, No. Ⅱ, No. Ⅴ and No. Ⅶ. Among them No. Ⅶ ore body is located to the northeastern end of the mine between 523~547 exploration lines and is 480m in total length.
机译:夏甸金矿位于著名的宜舒断裂带的东侧,构造性地位于鲁东(山东东部)上升(第二级构造单元)的胶北隆起(第三级构造单元)中。在该矿的东南侧发现了Ar-chean Jiaodong组的变质岩,第四纪沉积物几乎没有分布。矿山的火成岩主要是罗家河黑云母花岗岩,并暴露于矿山的西北部。该矿的控矿构造主要以断层为特征,招远—平度(昭平)断层带贯穿该矿。招远-平度断裂带的中段,即直下-江家窑断裂及其次生及相关断裂,构成了该矿的控矿构造。夏甸金矿床由西南向东北,由四个矿体组成。 Ⅰ,Ⅱ,Ⅴ,and号。其中Ⅶ矿位于矿山东北端,位于523〜547条勘探线之间,全长480m。

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