营口鲅鱼圈望海寨钼矿床地质特征及矿床成因探讨

The Molybdenum Ore Character and Formation Discussing of Bayuquan Wanghai

辽宁省营口鲅鱼圈望海寨钼矿床为侵入岩浆热液矿床,钼矿脉赋存于大望海寨花岗岩岩系及其外接触带上。钼矿床的形成有其特定的地质条件,尽管钼矿床的类型和规模各有其特点,但有一定的规律可循。望海寨钼矿床与区域地质构造条件有密切联系,通过研究和探讨钼矿床的形成原因,能够认识钼矿床成矿规律,以指导今后找矿工作。

Wanghaizhai molybdenum ore is located in Yingkou, Liaoning Province, which is a magmatic intrution and hydrothermal deposit. Molybdenum-vein is in the Da Wanghaizhai granite rock series and outside contact belt, Molybdenum deposit is formed by special geologicalen vironment. Although the type and the size of molybdenum deposit has characteristics, but it has a certain regularity to follow. Molybdenum deposit has close relation to the regional geological structure. By studying and discussing about the formation of the molybdenum deposit, we＇ll able to understand the regularity. It has meanings in theory and practice that in order to explore and harness mineral resource.