四川省攀西裂谷成矿带成矿地质特征及找矿方向  

The geological characteristics and ore seek direction of Panxi rift valley minerogenic belt in Sichuan province

作　　者：李建忠[1] 胡琴霞 余金元 杨福立 南争路 

机构地区：[1]中国人民武装警察部队黄金第十二支队,四川成都610036

出　　处：《中国矿业》2013年第5期69-72,103,共5页China Mining Magazine

摘　　要：攀西裂谷成矿带经历了长期的地质历史演化,地层出露齐全,构造活动强烈,岩浆活动频繁,变质作用复杂,产出了丰富的矿产资源,素有"矿产资源聚宝盆"的美誉,是近年来地质找矿和科学研究的热点地区。为了加强我部在四川的找矿力度,研究攀西地区的成矿规律,总结成矿富集规律,进行成矿预测,优选有利找矿靶区开展地质找矿工作,对指导找矿突破具有重要意义。Panxi rift valley minerogenic belt was evented long-term geologic history evolution, stratum basset complete, structure activity intensity, magma activity frequent, metamorphism complex, output abundant mineral resources, usually have ＂mineral resources cornucopia＂ praise, nearly, is the hotspot of the geologic seek ore and prescientific, to be enhance Sichuang Province seek ore work, research of Panxi metallogenic regular and generalize metallogenic beneficiation regular,carry through metallogenic prognosis, selective preference avail metallogenic prognosis zone to carry through Geology work,to supervise seek ore work breach have importance meaning.

关 键 词：地质特征 成矿预测 找矿方向 攀西裂谷成矿带 

分 类 号：P56[天文地球—构造地质学] P71[天文地球—地质学]