地质与资源2018，Vol.27Issue(3)：243-250,8.
小兴安岭霍吉河钼矿床成矿过程——透岩浆成矿作用
ORE-FORMING PROCESS OF THE HUOJIHE MOLYBDENUM DEPOSIT IN XIAOXINGANLING MOUNTAINS: Transmagmatic Mineralization
摘要
Abstract
Traditionally, the Huojihe molybdenum deposit in Xiaoxinganling Mountains is classified as porphyry type. With study on its geological characteristics such as non-porphyritic mass, orebodies circling around the cryptoexplosive breccia, veinlet-network and disseminated structures of quartz and the metallogenic age obviously later than forming time of host rock, it is believed that the deposit is formed by transmagmatic mineralization. The large-super large molybdenum deposit associated with the Early Mesozoic Yichun-Yanshou granitic batholith belt is a typical product of post-batholith metallogenesis.关键词
霍吉河钼矿床/隐爆角砾岩/透岩浆成矿/后岩基成矿/小兴安岭Key words
Huojihe molybdenum deposit/cryptoexplosive breccia/transmagmatic mineralization/post-batholith metallogenesis/Xiaoxinganling Mountains分类
天文与地球科学引用本文复制引用
王泉,刘东舟,郭鸿斌..小兴安岭霍吉河钼矿床成矿过程——透岩浆成矿作用[J].地质与资源,2018,27(3):243-250,8.基金项目
黑龙江省国土资源厅物化探异常查证项目"黑龙江省伊春异常查证区(2016)化探异常查证"(KCZX-YCCZ-2016005). （2016）
