摘要
得尔布干成矿带中段八大关—新峰山地区断裂构造发育 ,北东向得尔布干深大断裂是重要的控岩控矿构造。与成矿有关岩浆岩主要为燕山期的中性—中酸性侵入岩及次火山岩。赋矿层位主要有上库力组、塔木兰沟组及谢尔塔拉组。在分析典型矿床的成矿地质特征基础上 。
A discusion is made on the metallogenic conditions on Badaguan Xinfengshan,the middle section of Derbugan Metallogenic zone,i.e,the ore controlling structure,the related strata to the mineral deposits,and the magma genesis.It is analized on the metallogenic ore forming character of the typical deposit and the prospecting direction is pointed out.
出处
《矿产与地质》
2002年第2期70-73,共4页
Mineral Resources and Geology
关键词
金属矿产
成矿条件
找矿预测
得尔布干成矿带
metallic mineral resoureces
metallogenic condition
prospect predicting
Derbugan metallogenic zone
