摘要
玉龙铜(钼)矿区是受岩浆热液作用和气液交代作用形成的典型斑岩—矽卡岩复合型矿床。在收集和阅读前人研究成果和技术资料的基础上,结合工作实践,通过对矿床的基本地质特征、成矿背景、矿化类型、围岩蚀变以及控矿条件和成矿作用等因素进行探讨,得出了该矿床的大体成矿过程,解释了玉龙铜(钼)矿区Ⅰ、Ⅱ、Ⅴ号矿体不同的成因背景和特征,并在此基础上建立了早期以斑岩—热液体系为核心,晚期以中低温热液—地下水对流循环为主的复合型成矿模式,为西藏三江地区同类矿床的寻找和勘查提供依据和指导。
Yulong Cu （Mo） Deposit is a typical porphry-skarn composite deposit, which is formed in the mag- matie hydrothermal and gas-liquid metasomatism. Based on systematic collection and review of previous studies of Yulong Deposit, combined with the working practice, and through the deposit basic geological characteristics, met- allogenic backgrounds,mineralization types, wall-rock alterations, ore-controlling conditions and mineralization fac- tors,the general ore-forming process and model were studied in this paper. At the same time, the different forming backgrounds and featuresof the I , II , V Ore-bodies of Yulong Cu（Mo） Deposit were explained. And based on the former studies, the porphyry-hydrothermal system was established as the core of mineralization model during the early stage, the convective circulation of low to moderate temperature hydrothermal-groundwater as the main com- posite mineralization model in late stage. Meanwhile, it provided theoretical foundation and indicative function for the same type of deposits finding and exploration in Sanjiang Area in Tibet.
出处
《有色金属（矿山部分）》
2013年第1期66-69,共4页
NONFERROUS METALS(Mining Section）
关键词
玉龙铜(钼)矿床
斑岩
岩浆热液
Yulong Cu（Mo）depositl porphry rockl magmatic hydrothermal
