摘要
早子沟金矿位于甘南藏族自治州境内,区内水系比较发育,气候为青藏高原高寒湿润气候区。地下水化学类型简单,主要为HCO_3-Ca-Mg型淡水。该矿床为裂隙充水矿床;通过对该矿床充水因素的分析和矿坑涌水量的预测,为矿山安全生产提供科学依据。
Zaozigou gold is located in Gannan Tibetan autonomous prefecture,the region's water system is relatively developed,the climate is the plateau of the Qinghai-Tibet plateau and humid climate. The type of groundwater chemistry is simple,mainly HCO_3-Ca-Mg fresh water. The deposit is a liexi mineral deposit. It provides scientific basis for the safety production of mine by analyzing the water-filling factors of the mine bed and the prediction of the water flow.
引文
[1]谢先明,徐标,周志华,等.某花岗岩地区地下水径流模数变化原因初探[J].地下水,2011,33(03):23-26.
[2]张卫雄,王有权,张惠清,等.玛曲格尔科金矿矿区水文地质特征及涌水量预测[J].甘肃地质学报,2009,18(03):61-66.