摘要
研究认为下水铅锌矿床为喷流沉积 +区域变质 +部分岩浆热液迭加的多因复成铅锌矿床 ,查明了矿床的控矿因素 。
It is considered that Xiashui lead zinc deposit is a complicated lead zinc deposit of multiple origins of effusive sedimentation plus regional metamorphism overlapped by magmatic hydrothermal fluid. The ore controlling factors, exploration indications and directions have been made clear.
出处
《矿产与地质》
2002年第5期287-290,共4页
Mineral Resources and Geology
