Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer

	Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer
	J.-T. Peng; R.-Z. Hu; P.G. Burnard
	2003
Source Publication	Chemical Geology
Volume	200 Issue:1-2 Pages:129-136
Indexed By	SCI
Language	英语
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/352002/4709
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	J.-T. Peng,R.-Z. Hu,P.G. Burnard. Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer[J]. Chemical Geology,2003,200(1-2):129-136.
APA	J.-T. Peng,R.-Z. Hu,&P.G. Burnard.(2003).Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer.Chemical Geology,200(1-2),129-136.
MLA	J.-T. Peng,et al."Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer".Chemical Geology 200.1-2(2003):129-136.

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