摘要
研究区位于大兴安岭成矿带中段,是黑龙江省重要的成矿带之一。依据研究区内已发现Cu矿体赋存特征,围岩蚀变类型等,确定为矽卡岩型CuFe矿(点),并与区域上该类型矿产成矿期次相同,预示深部具有(多宝山式)斑岩型矿可能性。
The study area is located in the middle of Greater Khingan range metallogenic belt, and is one of the important metallogenic belts in Heilongjiang province. On the basis of the study area have been found Cu orehody occurrence characteristics, rock alteration types, identified as skam ore Cu-Fe, and the types of mineral resources and regional metallogenic period, has the possibility of porphyry deposit in deep part（ Duobaoshan type）.
出处
《甘肃冶金》
2018年第2期76-78,85,共4页
Gansu Metallurgy
关键词
区域地质背景
找矿潜力
八直沟地区
黑龙江
regional geological background
prospecting potential
Bazhigou area
Heilongjiang
