摘要
波风岭石墨矿是陕西省太白—商南石墨成矿带上新发现的一个大鳞片石墨矿。石墨矿赋存于古元古界秦岭群雁岭沟组黑云斜长片麻岩、石墨大理岩中,矿床类型为区域变质型,与全国主要的晶质石墨矿床类型和成矿时代一致。对波风岭石墨矿的地质特征全面分析,总结其矿床成因,对于在秦岭地区寻找同类矿床具有参考意义。
Bofengling graphite deposit is a newly discovered large scale graphite deposit in Taibai - shangnan graphite metallogenic belt of Shaanxi province. Graphite deposits occur in the dark cloud gneiss and graphite marble of the yanlinggou formation of the Qinling group in the paleoproterozoic. the type of deposits is of regional metamorphic type, which is consistent with the major types of crystalline graphite deposits in the country and the age of mineralization. An overall analysis of the geological characteristics of the Fengling graphite deposit and a summary of its genesis are of guiding significance for finding similar deposits in the Qinling region.
作者
杨联涛
YANG Lian-tao(Shaanxi Branch of China Geological Exploration Center of Building Materials Industry,Xi’an 710003)
出处
《矿产勘查》
2019年第2期257-263,共7页
Mineral Exploration
基金
陕西省商洛市沙河子-峦庄-带晶质石墨矿调查评价(编号:DD20160058-08)资助
关键词
石墨矿
地质特征
波风岭
陕西
graphite deposit
geological charactereristics
Bofengling
Shaanxi
