摘要
研究区位于黑龙江省东北部,多宝山铜金钼钨成矿带南部,是我国著名的斑岩型铜金钼矿成矿区。本次研究通过对矿区地质特征、成矿作用进行系统的地质调查,并结合区域物探分析进一步的找矿方向,阐明本区金的成矿与北东向的构造的关系,研究表明:北东向构造是本区最重要的导矿和容矿构造,为含矿热液的运移及形成提供了有利的空间。
The study area is located in northeastern Heilongjiang Province, which is in the south of Duobaoshan copper-gold and molybdenum tungsten mineralization belt, is the well-known copper-gold porphyry molybdenum ore mineralization area. Through systematic geological survey of geological features and mineralization, combining with regional geophysical for further prospecting direction, the authors clarified the relationship between mineralization and the NE structure of the district. The study showed that NE structure is the most important of lead and host structure, which provide a favorable environment for migration and formation of ore-bearing hydrothermal fluid.
出处
《吉林地质》
2016年第2期27-29,共3页
Jilin Geology
关键词
地质特征
成矿作用
金矿
永新北
geological features
mineralization
gold ore
North Yongxin
作者简介
王国琦（1992-），男，黑龙江齐齐哈尔人，河北地质大学在读硕士研究生．
