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内蒙古达来敖包钼多金属矿地质特征及找矿潜力浅析 被引量:5

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摘要 达来敖包钼多金属矿赋存在深部细粒花岗岩外接触带宝力高庙组变质粉砂岩、细砂岩内。钼矿化与北东向构造裂隙或构造破碎带有关,矿化体呈细脉状。矿体及围岩中,云英岩化、硅化、黄铁矿化比较强烈,并在细粒花岗岩外接触带发育,表明与岩浆热液的多次活动有关,属热液型矿床。通过目前勘查程度,达中——大型钼矿,分析其成矿地质特征、地球物理特征、地球化学特征、成矿地质环境等,认为深部及外围找矿潜力巨大。
出处 《西部资源》 2014年第2期102-105,共4页 Western Resources
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