以安徽池州市南自来山铜钼矿床为例浅析界面成矿模型对找矿预测的意义  

In Anhui Chizhou mountain to Nanzi copper molybdenum deposit metallogenic model of interface of ore prospecting significance

作　　者：曾全 

机构地区：[1]安徽地矿局321地质队,安徽安庆244033

出　　处：《世界有色金属》2017年第14期141-142,共2页World Nonferrous Metals

摘　　要：界面成矿在成矿作用过程中十分重要。O/S界面是很重要的热液交代成矿结构面,经常形成沿界面产出的规模大的似层状矿体。南自来山铜钼矿矿体主要产出于O/S界面位置,是典型的O/S界面成矿。通过对南自来山铜钼矿床的分析浅析界面成矿在找矿预测中的重要作用。Interface mineralization is very important in the process of mineralization. The O/S interface is an important hydrothermal metasomatic metallogenic structural surface, often forming a large size of stratiform ore deposits along the interface. South Mountain Copper Molybdenum ore body mainly in the position of the O/S output interface, O/S interface is a typical mineralization. Based on the analysis of the Cu Mo deposit, it is concluded that the metallogenic process plays an important role in ore prospecting.

关 键 词：南自来山铜钼矿床 O/S界面 界面成矿 找矿预测 

分 类 号：P618.41[天文地球—矿床学]