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Sm-Nd isotope dating of hydrothermal calcites from the Xikuangshan antimony deposit, Central Hunan
Jiantang Peng; Ruizhong Hu; Yuanxian Lin; Junhong Zhao
2002
Source PublicationChinese Science Bulletin
Volume47Issue:13Pages:1134-1137
metadata_24其它
AbstractThe research on Samarium-Neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit, Central Hunan, places precise timing constraints on the Sb mineralization in this area. It is revealed that the Xikuangshan deposit formed during the late Jurassic-early Cretaceous Period, the early- and latestage mineralization took place at (155.5 ± 1.1) Ma and (124.1 ±3.7) Ma, respectively. The accurate age determination of mineralization is very crucial for revealing the super- enrichment mechanism of the element Sb at the Xikuangshan mine, and lays some foundations for the further understandings of its ore genesis and mineralization mechanism.
KeywordMineralization Epoch Sm-nd Isotope Systematics Hydrothermal Calcites Xikuangshan Antimony Deposit.
Subject Area矿床地球化学
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/3109
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
Recommended Citation
GB/T 7714
Jiantang Peng,Ruizhong Hu,Yuanxian Lin,et al. Sm-Nd isotope dating of hydrothermal calcites from the Xikuangshan antimony deposit, Central Hunan[J]. Chinese Science Bulletin,2002,47(13):1134-1137.
APA Jiantang Peng,Ruizhong Hu,Yuanxian Lin,&Junhong Zhao.(2002).Sm-Nd isotope dating of hydrothermal calcites from the Xikuangshan antimony deposit, Central Hunan.Chinese Science Bulletin,47(13),1134-1137.
MLA Jiantang Peng,et al."Sm-Nd isotope dating of hydrothermal calcites from the Xikuangshan antimony deposit, Central Hunan".Chinese Science Bulletin 47.13(2002):1134-1137.
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