摘要
针对中条山南和沟铜矿床地质特征,通过对成矿大地构造背景、地层、构造及火山活动对成矿的控制作用的研究,表明南河沟矿床受剥离断层和变质热液双重成矿作用控制,具多因素成矿特征。
According to the geological characteristics of the Nanhegou copper deposit in Zhongtiaoshan, the study has analyzed how the tectonic background, strata, structure and volcanic movements controlled the ore-forming process, and pointed out that the mineralization of Nanhegou deposit was double controlled by stripping faults and metamorphic hydrotherm. The studying deposit was formed from different factors.
出处
《矿产与地质》
2008年第6期525-527,共3页
Mineral Resources and Geology
关键词
铜矿床
剥离断层
变质热液
南和沟
中条山
山西
copper deposit, stripping fault, metamorphic hydrotherm, Nanhegou, Zhongtiaoshan, Shanxi
