摘要
龙山地区铜多金属矿处于雪山峰-布尔汉布达华力西-印支期钴、金、铜、玉石(稀有、稀土)成矿带,区内构造活动强烈,北西向或近东西向断裂为区内重要的控矿构造,通过1∶5万水系沉积物,1∶1万土壤测量等工作,综合分析了区内地质地球化学特征,查明区内元素的分布规律和组合特征,圈定了三条矿化蚀变带,三条矿(化)体,并初步查明了矿体的形态、产状和规模。研究表明,该区具备良好的成矿地质条件,成矿潜力较大,具有良好的找矿前景。
The copper-polymetallic deposits in Longshan area is located in the snow mountain,Boolean han buda variscan,indosinian period of cobalt,gold,copper and jade(rare,rare earth)metallogenic belt,strong tectonic activities in the area,north west or nearly east-west fracture is the important ore-controlling structures,through the 1∶50 000 stream sediment and soil of 1∶1 000 000 measurement work,comprehensive analysis of the geological and geochemical characteristics in this area,we find out the distribution of elements in the area and characteristics of combination and delineated the three mineralized alteration zone,three mines,and find out the orebody shape,occurrence and scale.Research shows that the good ore-forming geological conditions,mineralization potential is bigger,has good ore prospects.
出处
《中国矿业》
北大核心
2017年第S1期180-184,共5页
China Mining Magazine
关键词
地球化学特征
找矿前景
铜多金属矿
龙山地区
geochemical characteristics
prospecting prospect
copper-polymetallic deposit
Longshan area
