新疆哈密黑山金矿点地质特征及找矿方向

Geological characteristics and prospecting orientation of Heishan gold ore deposit in Hami city,Xinjiang Province

黑山金矿处于阿其克库都克-沙泉子断裂以南的卡瓦布拉克-星星峡地块,由天湖岩群变质岩和晚古生代中酸性火山岩组成矿床发现于2016年,2017年-2018年通过钻探工程,对金矿(化)带进行了验证,本文介绍了矿点地质特征、总结了找矿标志,初步认为其成因为浅成低温热液型,该区工作程度低,结合综合研究成果,指出了矿化带的西南、东北方向以及深部为下一步的找矿方向。

The Heishan gold occurrence which is located in the plot of Kawabulake-XingXingXia in the south of Archik koduk-Shaquanzi fault and composed of shallow metamorphic rocks of Tianhu Group and late Paleozoic acidic volcanic rock, is found in 2016. Orebodies are verified by drilling engineering in 2017 and 2018. This paper introduces the geological characteristics and summarizes indicators for the gold occurrence. It is preliminarily believed that the gold occurrence is the hydrothermal type of hypabyssal low temperature, and the degree of work in this area is low, it is pointed out that the southwest, northeast and deep of the mineralized zone are the next prospecting direction by comprehensive research.