摘要
杨梅田铜多金属矿在其近几十年的找矿探矿史上,一直未取得重大的突破。本文通过对矿区从区域到矿床的地质特征进行细致的研究,认为杨梅田铜多金属矿属于典型的构造热液型脉状矿床,矿体的产出受地层岩性、断裂构造和热液控矿等控制因素的影响,为矿区的找矿探矿工作提供一定的指导和参考作用。
Yangmeitian copper polymetallic ore has not made major breakthroughs in its history of exploration and prospecting in recent decades. It is believed that Yangmeitian copper polymetallic ore is a typical tectonic hydrothermal vein deposit through a detailed study on the geological characteristics of the mining area from the area to the deposit. And the output of ore bodies is affected by controlling factors such as stratum lithology, fault structure and hydrothermal ore control, provide some guidance and reference for the exploration and prospecting work in the mining area.
作者
吕品翰
王家仁
谢恩彩
李俊
陈飞
LV Pin-han;WANG Jia-ren;XIE En-cai;LI Jun;CHEN Fei(Faculty of Land Resource Engineering,Kunming University of Science and Tedchnology,Kunming 650032,China;Yongchang Pb&Zn Co.,Ltd.,Baoshan 678307,China)
出处
《价值工程》
2019年第4期92-95,共4页
Value Engineering
关键词
杨梅田铜多金属矿
构造热液型脉状矿床
怒江大断裂
充填交代
Yangmeitian copper polymetallic ore
structural hydrothermal vein deposit
nujiang great fault
filling-metasomatism
