摘要
通过对与沙让钼矿成因有关的地层与岩性、岩浆岩、构造、矿化及围岩蚀变、矿体特征等分析,认为沙让钼矿受地层、花岗斑岩体、构造控制,矿体特征明显,矿化蚀变发育,且分带清楚,矿床成因为斑岩型钼矿床。
This paper indicates the Sharang molybdenum deposit＇s genesis is porphyry-type molybdenum deposit through analyzing its the layer and lithology,magmatitc rock,tectonics,mineralization,wallrock alteration and orebody characters relations with genesis of the Sharang molybdenum deposit.
出处
《资源环境与工程》
2011年第1期29-32,共4页
Resources Environment & Engineering
关键词
沙让
钼矿
矿床成因
Sharang
molybdenum deposit
genesis of deposit
