摘要
斑岩型金矿是我国第三重要的金矿类型,但目前对其认识程度远不如其他类型金矿,尤其关于它的亚类划分。依据斑岩金的共生元素或组合及矿石类型,将斑岩型金矿划分为三个亚类:伴生斑岩型金矿、共生斑岩型金矿和独立斑岩型金矿。斑岩型金矿的成矿“深度相”目前认识不一。笔者认为,其主体在近地表—浅成(近地表1.5km)范围内。我国独立斑岩型金矿的矿质硫和铅,其主体与和它们时空相随、成因相关的火成岩同源,属壳幔混合源或下地壳源。
The porphyry gold deposit is an important type both at home and abroad,but study on it is far less than those on other types of gold deposits.The name of porphyry gold deposit is based on both deposit industrial type.Authors suggest in this paper that porphyry gold deposit be classified as associated,coexisting and independent porphyry gold deposit.China metallogenetic depth facies of porphyry gold deposit is stretch from nearsurface to hypabyssyl,0.1~3 km depth. Mineral S and Pb of Yuerya and Zijinshan both porphyry gold deposits come from the igneous rock related in, and genesis.
出处
《世界地质》
CAS
CSCD
1999年第1期16-20,38,共6页
World Geology
关键词
斑岩型金矿
分类
成矿深度相
矿质来源
金矿床
porphyry gold deposit, classification, metallogenetic depth facies, source