节点文献
内蒙古克什克腾旗哈尔楚鲁图银多金属矿区矿床成因及找矿标志
The Genesis and Prospecting Mark of the Halchulutu Silver Polymetallic Deposit in Keshiketengqi,Inner Mongolia
【摘要】 通过对内蒙古克什克腾旗哈尔楚鲁图银多金属矿区成矿地质背景、矿床(体)地质特征、矿物组合类型等进行分析研究,认为区内矿体严格受北西向构造控制,矿床成因类型为岩浆期后中-低温热液充填式脉状铅锌多金属矿床,并提出本区的找矿标志,以指导矿区勘查工作。
【Abstract】 This paper analyzes and studies the metallogenic geological background,the geological features and the types of mineral associations in the Halchulutu silver polymetallic ore district of Heshiketengqi,Inner Mongolia. It is believed that the orebodies in the area are strictly influenced by the northwestern structure. Control,the type of genetic deposit is a postmagmatic low-temperature hydrothermal-filled pulsed lead-zinc polymetallic deposit in the magmatic stage,and the prospecting signs in this area are proposed to guide the exploration work in the mining area.
【关键词】 哈尔楚鲁图;
矿体特征;
矿床成因;
找矿标志;
【Key words】 Halchulutu; orebody characteristics; origin of deposits; ore-prospecting sign;
【Key words】 Halchulutu; orebody characteristics; origin of deposits; ore-prospecting sign;
- 【文献出处】 甘肃冶金 ,Gansu Metallurgy , 编辑部邮箱 ,2018年04期
- 【分类号】P618.2
- 【被引频次】2
- 【下载频次】43