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锡矿山锑矿床热液方解石的Sm—Nd同位素定年
彭建堂; 胡瑞忠; 赵军红; 林源贤
2002
Source Publication科学通报
Issue10Pages:789-792
Other Abstract通过对热液成因方解石Sm-Nd同位素体系的研究,对湘中锡矿山超大型锑矿床的形成时代进行了精确限定.研究表明,锡矿山锑矿床形成于晚侏罗世~早白垩世,早、晚两期的成矿作用时间分别是(155.5±1.1)和(124.1±3.7)Ma.对该矿床成矿时代的精确厘定,有助于揭示该区元素Sb的超常富集机制,为深入认识其矿床成因和成矿机理奠定了基础. 
Keyword成矿时代 Sm-nd同位素体系 热液方解石 锡矿山锑矿床
Subject Area矿床地球化学
Indexed BySCI
Language中文
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/6726
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彭建堂
Recommended Citation
GB/T 7714
彭建堂,胡瑞忠,赵军红,等. 锡矿山锑矿床热液方解石的Sm—Nd同位素定年[J]. 科学通报,2002(10):789-792.
APA 彭建堂,胡瑞忠,赵军红,&林源贤.(2002).锡矿山锑矿床热液方解石的Sm—Nd同位素定年.科学通报(10),789-792.
MLA 彭建堂,et al."锡矿山锑矿床热液方解石的Sm—Nd同位素定年".科学通报 .10(2002):789-792.
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