| 青海东昆仑督冷沟铜钻矿床控矿条件的探讨 |
| |
| 引用本文： | 潘彤.青海东昆仑督冷沟铜钻矿床控矿条件的探讨[J].矿产与地质,2004,18(2):109-112. |
| |
| 作者姓名： | 潘彤 |
| |
| 作者单位： | 吉林大学地球科学学院 长春130061，青海有色地质勘查局，西宁810007 |
| |
| 摘 要： | 督冷沟铜钻矿床位于近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。
|
| 关 键 词： | 铜钴矿床 控矿条件 探讨 督冷沟 青海东昆仑 |
| 文章编号： | 1001-5663(2004)02-0109-04 |
| 修稿时间： | 2003年11月13 |
DISCUSSION ON ORE CONTROLLING CONDITION OF DULENGOU Cu-Co DEPOIST IN EASTERN KUNLUN METALLOGENIC BELT,QINHAI |
| |
| PAN Tong.DISCUSSION ON ORE CONTROLLING CONDITION OF DULENGOU Cu-Co DEPOIST IN EASTERN KUNLUN METALLOGENIC BELT,QINHAI[J].Mineral Resources and Geology,2004,18(2):109-112. |
| |
| Authors: | PAN Tong |
| |
| Abstract: | 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. |
| |
| Keywords: | Cu-Co deposit ore controlling conditions discussion Dulengou Kunlun |
| 本文献已被 CNKI 维普 等数据库收录！ |
