节点文献
甘肃省张家川县秦家园铅锌矿地质特征及矿床成矿模式探讨
Geological characteristics and metallogenic model of qinjiayuan pb-zn deposit in zhangjiachuan county gansu province
【摘要】 秦家园铅锌矿床赋存于长城系陇山群地层中,受北北东向断裂构造控制。矿石工业类型地表均为铅锌氧化矿石,地表向下垂高80m以下多为混合或原生矿石。矿石结构主要为碎裂状结构;团块状构造。矿石矿物主要为闪锌矿、方铅矿及其氧化物。具典型的中低温热液充填-交代型矿床特点。具有深部找矿的潜力。
【Abstract】 The Qinjiayuan lead-zinc deposit occurs in the Longshan Group strata of the Great Wall System and is controlled by NE-trending faults. The surface of the ore industry type is lead-zinc oxide ore, and most of the ore below 80 m vertical is mixed or primary ore. The ore structure is mainly fractured structure and massive structure. The ore minerals are sphalerite,galena and their oxides. The deposit has typical characteristics of medium-low temperature hydrothermal filling-metasomatic type. It has deep prospecting potential.
【关键词】 秦家园铅锌矿床;
地质特征;
矿床成矿模式探讨;
【Key words】 Qinjiayuan lead-zinc deposit; geological characteristics; metallogenic model of the deposit;
【Key words】 Qinjiayuan lead-zinc deposit; geological characteristics; metallogenic model of the deposit;
- 【文献出处】 世界有色金属 ,World Nonferrous Metals , 编辑部邮箱 ,2019年02期
- 【分类号】P618.42;P618.43
- 【网络出版时间】2019-04-04 14:33
- 【下载频次】21