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吉林磐石市兴隆沟金矿床地质特征
引用本文:单承恒,姜建军,王忠义,赵光剑.吉林磐石市兴隆沟金矿床地质特征[J].吉林地质,2009,28(3):18-22,42.
作者姓名:单承恒  姜建军  王忠义  赵光剑
作者单位:1. 吉林省有色金属地质勘查局六〇七队,吉林,吉林市,132105
2. 吉林省有色金属地质勘查勘查院,吉林,长春,130021
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。

关 键 词:金矿  岩浆岩  构造  矿化特征  兴隆沟  磐石  吉林

Geological features of Xinglonggou gold deposit of Panshi, Jilin Province
SHAN Cheng-heng,JIANG Jian-jun,WANG Zhong-yi,ZHAO Guang-jian.Geological features of Xinglonggou gold deposit of Panshi, Jilin Province[J].Jilin Geology,2009,28(3):18-22,42.
Authors:SHAN Cheng-heng  JIANG Jian-jun  WANG Zhong-yi  ZHAO Guang-jian
Institution:SHAN Cheng-heng, JIANG Jian-jun WANG Zhong-yi, ZHAO Guang-jian(1. Team 607, Non-ferrous Metal Geology Prospecting Bureau of Jilin Province, Jilin 132105, China 2. Institute of Non-ferrous Metals Geological Exploration of Jilin Province, Changchun 130021, Jilin, China)
Abstract: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.
Keywords:gold deposit  magmatie rock  structure  mineralization characteristics  Xinglonggou  Panshi  Jilin
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