摘要
兴隆沟金矿区位于天山—兴安地槽褶皱系,吉林优地槽褶皱带,吉林复向斜,双阳—磐石褶皱束南东段,辉发河深大断裂北侧槽区边缘。为金及多金属的重要成矿区。文章通过对构造运动、岩浆岩分布特征及其与成矿作用的关系的研究,指出了构造、岩浆活动在成矿过程中起着重要作用。文中分析的岩浆岩与构造作用,对扩大矿区的找矿规模意义重大。
Xinglonggou gold deposit occurs in Tianshan-Xing＇an geosynclinal＇s folds, Jilin eugeoyncline fold belt, Jilin synclinoria, eastsouth part of Shuangyang-Panshi fold cluster, north margine of the Huifahe deep fault, which is an important metallogenic province for gold and polymetallic ores. According to studying on the structural movement, magmatic distribution and mineralization, it indicates the importance of the structural processes and magmatic activities tbr the ore-forming.
出处
《吉林地质》
2009年第3期18-22,42,共6页
Jilin Geology
关键词
金矿
岩浆岩
构造
矿化特征
兴隆沟
磐石
吉林
gold deposit
magmatie rock
structure
mineralization characteristics
Xinglonggou
Panshi
Jilin
