摘要
巴希库勒稀有金属矿位于霍拉山,大地构造位置属于南天山-霍拉山陆缘裂谷。稀有金属矿体产出于含绿柱石伟晶岩脉中,多分布于石炭纪侵入体与晚元古代花岗片麻岩接触带附近,成因类型属花岗伟晶岩型稀有金属矿床。
The bashikule rare metal deposit is located in the Huola mountain,and the geotectonic location belongs to the South Tianshan Huola mountain continental margin rift.The rare metal ore bodies are mainly distributed near the contact zone between Carboniferous intrusive body and late Proterozoic granitic gneiss,and belong to granitic pegmatite type rare metal deposits.
作者
杨智全
YANG Zhi-quan(The Third Geological Brigade of Xinjiang geological and mineral exploration and Development Bureau,Korla 841000,China)
出处
《世界有色金属》
2019年第23期104-105,共2页
World Nonferrous Metals
关键词
霍拉山
巴希库勒稀有金属矿床
地质特征
成因类型
Huola mountain
bashikule rare metal deposit
geological characteristics
genetic type
