摘要
督冷沟铜钴矿床位于近EW向东昆仑构造带东段,它形成于晚古生代岛弧环境,成矿地质作用非常复杂,绿泥绢云母千枚岩为主要赋矿地层,构造变形使矿质运移、富集。认为该矿床控矿条件为地球动力学环境、变质火山岩及构造变形综合控制。
The Dulengou Cu-Co deposit is located in the eastern area of Kunlun metallogenic belt. It was formed in the structural environment of island arc of late Palaeozoic Era. The ore bearing rock consits of late Cretaceous sericite quartz schist,later structural deformations enriched the ore body. The ore controlling factors are geodynamic mechanism,layer of volcanic rock,structurl deformations in Dulengou Cu-Co deposit.
出处
《矿产与地质》
2004年第2期109-112,共4页
Mineral Resources and Geology
关键词
铜钴矿床
控矿条件
探讨
督冷沟
青海东昆仑
Cu-Co deposit
ore controlling conditions
discussion
Dulengou
Kunlun
