摘要
紫金县锡多金属矿位于广东省紫金县境内,区内水系不发育,气候为亚热带季风气候区。地下水类型简单,主要为SO4-Ca·Mg型和HCO3-Mg型淡水,地下水的补给来源主要是大气降水,该矿床为裂隙充水矿床,充水矿床勘探的复杂程度划分为中等型,属水文地质条件中等矿床。
The tin polymetallic deposit is located in Zijin county, Guangdong province. The water systems in this district are not developed, while the climate here belongs to subtropical monsoon climate zone. The chemical type of groundwater is simple and mainly belongs to fresh water of SO4-Ca · Mg type or HCO3 -Mg type. Groundwater is the main source of atmos- pheric precipitation recharge. The deposit is a deposit of fissure filled with water. The complexity of the exploration of the water-filled deposit is classified to the medium type, belonging to a medium deposit in the hydrogeological condition.
出处
《甘肃冶金》
2016年第3期80-83,共4页
Gansu Metallurgy
关键词
锡多金属矿
水文地质
条件特征
tin polymetallic deposit
hydrogeology
condition feature
