摘要
通过对矿床地质特征、同位素地质学的研究，探讨了南岔金矿床的矿床成因、成矿温度和成矿时代。指出矿体受构造控制，成因上与燕山期岩浆侵入活动关系密切，并提出了南岔金矿床的成矿模式。
Based on the analyses on the geological features and stable isotope data,the genesis,temperature and epoch of Nancha gold deposit are discussed.Ore body is controled by structure,and mineralization has close relationship with Yanshan magma intrusion.Metallogenic model of Nancha gold deposit is established.
出处
《黄金地质》
1997年第3期36-41,共6页
Gold Geology
