GYIG OpenIR  > 矿床地球化学国家重点实验室  > 期刊论文
个旧超大型锡多金属矿稀土元素地球化学特征
贾润幸; 方维萱; 赫英; 高振敏; 李红阳
2005
Source Publication中国稀土学报
Issue2Pages:228-234
Other Abstract对比研究了个旧不同类型岩(矿)石(蚀变花岗岩、钙质泥岩、大理岩、矽卡岩矿石、层状矿石和脉状矿石)的稀土元素、微量元素地球化学特征,借以示踪不同类型矿床的成矿物质来源。研究表明不同类型矿石中的稀土元素配分曲线较为相似,成矿物质具有同源性,并与本区的花岗岩具有一定的成因联系。由于其成矿方式的不同,不同类型矿石中的稀土元素特征和矿物组合特征略有差异,脉状矿石和层状矿石中稀土含量相对较少且富集轻稀土,而矽卡岩矿石中稀土含量相对较多且轻、重稀土的含量变化较大。
Keyword稀土元素地球化学 锡多金属矿成因 稀土
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:1965467
Citation statistics
Cited Times:6[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/7463
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
贾润幸,方维萱,赫英,等. 个旧超大型锡多金属矿稀土元素地球化学特征[J]. 中国稀土学报,2005(2):228-234.
APA 贾润幸,方维萱,赫英,高振敏,&李红阳.(2005).个旧超大型锡多金属矿稀土元素地球化学特征.中国稀土学报(2),228-234.
MLA 贾润幸,et al."个旧超大型锡多金属矿稀土元素地球化学特征".中国稀土学报 .2(2005):228-234.
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