摘要
根据兰家沟钼矿区控矿旋卷构造特征、燕山期花岗岩体的岩石化学特征、稀土元素特征和成矿元素含量。
On the basis of the features of orecontrolling rotational structure in molybdenum mineral area of Lanjiagou district,lithochemical characteristics of granitic instrusive of Yanshan period and of rare earth elements,and content of metallogenic elements,it is discussed in this paper the role of the geological structure of the mineral area and the magmatic evolution and differentiation in the mineralizing process of the molybdnum deposit.
出处
《矿产与地质》
1999年第3期135-140,共6页
Mineral Resources and Geology
关键词
钼矿床
成矿构造
岩浆演化
成矿作用
Zone of subsidence in HebeiLiaoning,Rotational structure,Magmatic differentication,Lanjiagou
