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:9[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
矿床地球化学国家重点实验室
Corresponding Author胡瑞忠
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.
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