摘要
本文综述了呼兰群地层总体为下古生界,其中黄莺屯组(下段为矿床围岩)相当于寒武—奥陶系,小三个顶子组(为第Ⅲ岩带围岩)属志留—泥盆系;辉发河深断裂为导岩(矿)构造,北西向断裂为容岩(矿)构造,系统地探讨了红旗岭岩浆硫化铜镍矿床(1号、7号)成岩(矿)的地质特征。
Most of the Hulan group strata belong to an early Paleozoic Era,among them,theHuangyintun Formation is equivalent to the Cambrian-Ordovician,(Lower is a cotintryrocks). Xiaosandingzi Formation belongs to Silurian-Devonian system(Country rock of thethird rock belt),Huifahe deep faults are structures as passage ways for rock(ore)fluids, NWfaults are structures for rock(ore)housing.Metallogenic characteristics of the Hongqilingmagmatic sulfide copper-nickel deposits(No.1, No. 7)are systematically discussed,therefore,the genetic types of deposits are subdivided.
出处
《吉林地质》
1995年第3期17-30,共14页
Jilin Geology
基金
1990~1992年<红旗岭铜镍矿区地质背景成岩(矿)规律和找矿方向>合作项目
关键词
岩浆
岩体
镍矿床
铜矿床
地质特征
Hongqiling Rockbody No. 1 Rockbody No. 7 Geological featuresCopper-nickel deposit Genetic type of deposit