摘要
本区矿床成矿类型属岩浆热液裂隙充填石英脉型金矿,含矿石英脉主要受北西向断裂构造控制。通过野外和室内工作研究,确定本区成矿与晚古生代-中生代区域岩浆活动密切相关。文章讨论了矿床的成因和成矿作用,详细阐述了矿石种类,对未来找矿方向提出建议。
The metallogenic type of the deposit belongs to the magmatic hydrothermal fracture filling quartz vein type gold deposit, and the ore bearing quartz vein is mainly controlled by the NW trending fault structure. Through field and indoor work study, it is determined that the mineralization in tiffs area is closely related to the late Paleozoic Mesozoic magmatic activity. The genesis and mineralization of the deposit are discussed in this paper. Ore types are expounded in detail and suggestions for future prospecting are put forward.
作者
荆振刚
赵际新
周阳
孔伟思
JING Zhen-gang;ZHAO Ji-xin;ZHOU Yang;KONG Wei-si(Team 607,Bureau of Nonferrous Metals Geological Exploration of Jilin Province,Jilin 132013,Jilin,China)
出处
《吉林地质》
2018年第3期26-32,共7页
Jilin Geology
关键词
金属矿物
地质特征
断裂
金矿
矿床
Metallic minera
geological characteristics
fracture
gold mine
deposit
