摘要
本文介绍了祁漫塔格新发现石墨矿化点的成矿地质背景、地质特征和地球物理特征,探讨了矿床成因和找矿标志。该石墨矿化点赋存于奥陶-志留系滩间山岩群中的石英片岩、二云母石英片岩中,可作为东昆仑地区石墨矿新的找矿目标体。
This paper introduces the metallogenic background, geological features and geophysical characteristic＇of newly discov- ered graphite mineralization point in Qimantage, explores the genesis and prospecting criteria. The graphite mineralization point occurrence in quartz schist, mica quartz schist of Tanjianshan terrain in Ordovician System to Silurian System which Can be used as the new prospecting target body of graphite mine in East Kunlun.
作者
王盘喜
李兴良
朱黎宽
WANG Pan-xi Li Xing-liang ZHU Li-kuan(Zhengzhou Institute of Multipurpose Utilization of Mineral Resources, CAGS, Zhengzhou 450006 National Research Center of Multipurpose Utilization of Non-metallic Mineral Resources, Zhengzhou 450006, China Third Institute of Qinghai Geological Mineral Prospecting, Xining 810029, China)
出处
《中国非金属矿工业导刊》
2017年第3期34-36,44,共4页
China Non-Metallic Minerals industry
基金
中国地质调查局地质调查项目(编号:DD20160073)
关键词
石墨
矿化点
成因探讨
祁漫塔格
graphite
mineralization point
genesis
Qimantage
