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Fluid inclusion characteristics of the Xiejiagou gold deposit in Eastern Shandong province, China

机译:山东省东部谢家沟金矿床流体包裹体特征

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The Xiejiagou gold deposit, founded in 2001 with the resource of 37 t Au, locates in Zhaoyuan city, Shandong province, China. The previous gold exploration and geological studies in Shandong province mainly focus on the large-scale fracture fault belts such as the Zhaoyuan-Pingdu fault Jiaojia-Xincheng fault and Sanshandao fault. While the Xiejiagou gold deposit occurs 3.5Km west to the Zhaoyuan-Pingdu fault, controlled by its sub-fault and a ductile shear zone. So the discovery of this deposit is a great breakthrough in the gold exploration in Shandong province. This paper mainly introduces the newest research result on the temperature, composition, H-O isotope etc of the fluid inclusions in the Xiejiagou gold deposit, then discusses the origin and evolution of ore-forming fluid.
机译:谢家沟金矿位于中国山东省招远市,成立于2001年,资源量为37吨金。山东省以前的金矿勘探和地质研究主要集中在招远—平度断裂,焦家—新城断裂和三山岛断裂等大型断裂断裂带上。谢家沟金矿床位于赵元—平度断层以西3.5公里,受其次断层和韧性剪切带控制。因此,发现该矿床是山东省金矿勘探的重大突破。本文主要介绍谢家沟金矿床流体包裹体的温度,组成,H-O同位素等最新研究成果,然后探讨成矿流体的成因和演化。

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