摘要
大宝山矿床黄铁矿和闪锌矿特征元素,硫、铅同位素组成,原生晕分带特征,矿物气液包裹体测温,赋矿围岩元素丰度等方面的研究结果表明,它属岩浆期后热液成因。
The Dabaoshan deposit is a polymetallic deposit containing Mo, W, Cu, Pb and Zn. There is much controversy about the genesis of the deposit. In the early 1960s, it was considered as a meso-hypothermal deposit resulting from interstratified replacement. Recently, some other genetic models have been put forward, e.g. the strata-bound deposit model.Studies of the contents of characteristic elements in pyrite and sphalerite, the compositions of sulfur and lead isotopes, zoning of primary halos, homogenization temperatures for fluid inclusions in minerals from the deposit and element abundances in the strata led to a conclusion that the deposit is of post-magmatic hydrothermal origin.
出处
《地球化学》
CAS
1987年第1期27-35,共9页
Geochimica
