摘要
本文通过对西藏多龙矿集区地质背景、区域地球物理和区域地球化学特征的研究,以区内典型矿床之一——多不杂铜矿为代表,分析矿体特征,确定矿区主要成矿类型为斑岩型,以及它的成矿模式。
This article mainly through to the Tibetan dragon more ore concentration area geological background, geophysical and geochemical features in the region, with more than one of the typical deposits in the area- not miscellaneous copper, represented by analyzing the characteristic of ore body and determine the main mining area for porphyry mineralization type, and its metallogenic model.
出处
《世界有色金属》
2016年第7期180-181,共2页
World Nonferrous Metals
关键词
多龙矿集区
地球化学
成矿模式
特征
dragon more ore concentration area
the geochemical
metallogenic mode
characteristic
