GYIG OpenIR  > 矿床地球化学国家重点实验室  > 期刊论文
羟铟石研究的新进展
张宝贵; 张忠
Corresponding Author张宝贵
2002
Source Publication地质与勘探
ISSN0495-5331
Volume38Issue:6Pages:30-33
Abstract羟铟石(Jalindite)产在云南个旧马拉格锡石-多金属矿床氧化带中,是一种铟的次生矿物,镜下观察白色透明,均质体。折光率1.725±0.002,α0=7.9514×10^-7mm。主要粉晶谱线(nm):0.395(10),0.279(8),0.178(10),0.163(8),0.1325(7),0.1260(7),0.1200(8),0.1065(10)。电子探针8个测试点平均含铟69.34%,元素分析含H1.78%。计算OH30.26%,不含C,S,N。矿物成因和实验研究表明,羟铟石中铟来源于原生硫化物矿物,铟在氧化铁矿石中主要呈独立矿物,其他形式均占极次要地位。
metadata_83矿床地球化学国家重点实验室
Keyword羟铟石 锡石硫化物矿床 赋存形式 云南
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:1005936
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/903
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
Corresponding Author张宝贵
Recommended Citation
GB/T 7714
张宝贵,张忠. 羟铟石研究的新进展[J]. 地质与勘探,2002,38(6):30-33.
APA 张宝贵,&张忠.(2002).羟铟石研究的新进展.地质与勘探,38(6),30-33.
MLA 张宝贵,et al."羟铟石研究的新进展".地质与勘探 38.6(2002):30-33.
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