摘要
大青山金矿床位于北山古生代裂谷系,呈脉状、透镜状产于石炭系下统红柳园组下亚组含炭碎屑岩中,骆驼峰—大青山—险峰断裂带及其派生的断裂组为其提供了有利的导矿、容矿空间。矿化体中金的富集与石英脉的空间分布、矿石的结构构造、金属硫化物的含量、粒度有着密切的关系。
The gold deposit of Daqingshan lies in Paleozoic rift system of Beishan, occuring as vein and lefts at carbonceous elastic rock of Lower sub-formation of lower Carboniferous, and the fracture zone of the Luotuofeng-Daqingshan-Xianfeng and the related fracture are the ore-transportation and host space. The enrichment of the gold is closely related to the spatial distributon of the quartz vein, the fabric and structure of the ore, and the content and granularity of the metal sulfides.
出处
《地质找矿论丛》
CAS
CSCD
2003年第z1期84-87,共4页
Contributions to Geology and Mineral Resources Research
关键词
大青山金矿
地质特征
成矿条件
新疆
Daqingshan gold ore
geologic character
mineralization condition
Xinjiang
