GYIG OpenIR  > 矿床地球化学国家重点实验室  > 期刊论文
澜沧江断裂带走滑变形及与临沧锗矿的关系
王国芝; 胡瑞忠; 方维萱; 陶晓风
2001
Source Publication矿物学报
Issue4Pages:695-698
Other Abstract建立在对断裂带的变形特征、运动学特征和变形岩石年代学的综合研究表明 ,澜沧江断裂带是一条左旋走滑断裂带 ,左旋走滑始于 2 0Ma。印支地块由南向北运动和保山地块的向南挤出 ,主要是通过红河断裂、怒江断裂的右旋走滑和澜沧江断裂的左旋走滑共同调节来实现的。澜沧江断裂带的左旋走滑制约了临沧帮卖盆地的形成演化、盆地内的热水活动、锗的富集成矿和锗矿床的空间分布。
Keyword澜沧江断裂带 左旋走滑 变形年代学 新第三纪盆地 锗矿
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:690690
Citation statistics
Cited Times:7[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/7327
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation
GB/T 7714
王国芝,胡瑞忠,方维萱,等. 澜沧江断裂带走滑变形及与临沧锗矿的关系[J]. 矿物学报,2001(4):695-698.
APA 王国芝,胡瑞忠,方维萱,&陶晓风.(2001).澜沧江断裂带走滑变形及与临沧锗矿的关系.矿物学报(4),695-698.
MLA 王国芝,et al."澜沧江断裂带走滑变形及与临沧锗矿的关系".矿物学报 .4(2001):695-698.
Files in This Item:
File Name/Size DocType Version Access License
澜沧江断裂带走滑变形及与临沧锗矿的关系.(151KB) 开放获取LicenseView Application Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[王国芝]'s Articles
[胡瑞忠]'s Articles
[方维萱]'s Articles
Baidu academic
Similar articles in Baidu academic
[王国芝]'s Articles
[胡瑞忠]'s Articles
[方维萱]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[王国芝]'s Articles
[胡瑞忠]'s Articles
[方维萱]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 澜沧江断裂带走滑变形及与临沧锗矿的关系.pdf
Format: Adobe PDF
This file does not support browsing at this time
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.