摘要
火神庙钼矿床位于三川-栾川陷褶断带中,对矿床特点及成因进行了研究。研究发现,火神庙钼矿床形成于晚侏罗世,成矿物质来源于壳幔混源,严格受到燕山期侵入的斑状角闪石英二长岩的内外接触带控制,是典型的矽卡岩型钼矿床。
Huoshenmiao molybdenum deposit is located in Sanchuan-Luanchuan geotectogene and fault-fold belt.The paper studies the deposit characteristics and causes.The research finds that the Huoshenmiao molybdenum deposit was formed in the Late Jurassic,and the ore-forming materials originated from the mixed crust-mantle source.It is strictly controlled by the internal and external contact zones of the porphyritic amphibole quartz monzonite invaded during the Yanshanian.It is a typical skarn-type molybdenum deposit.
作者
张伟
欧路文
史保堂
陈飞
ZHANG Wei;OU Luwen;SHI Baotang;CHEN Fei(No.1 Institute of Geological and Mineral Resources Survey of Henan,Luoyang 471000;Henan Key Laboratory of Gold and Silver Polymetallic Mineralization Series and Deep Prediction,Luoyang 471000,China)
出处
《矿业工程》
CAS
2020年第1期4-8,共5页
Mining Engineering
