摘要
金堆城钼矿体已从上部开采到中部,矿区Mo的品位增高,辉钼矿的产出特征发生了相应的变化,晶体形态以板条状、叶片状及其集合体为主,嵌布粒度变粗,大于015mm的颗粒占到49%,矿体北部钼的氧化率降低。
The changes have taken place for the characteristic of molybdenite in Jinduicheng mine because the grade of molybdenum increasedThe crystal morphology appears board,blade and their aggregateThe dissemination size is thicker,49% grain is more than 0.15 m,and the molybdenum oxidation rate
出处
《中国钼业》
1998年第2期18-20,17,共4页
China Molybdenum Industry
关键词
辉钼矿
晶体形态
嵌布粒度
钼矿床
Molybdenite,Crystal morphology,Dissemination size,Molybdenum oxidation rate