Isotopic compositions of the peridotitic xenoliths from the Nushan area, Anhui Province: Constraints on the age of subcontinental lithospheric mantle beneath the East China | |
Liu ZhiChao1; Wu FuYuan1; Chu ZhuYin1; Xu XiSheng2 | |
刊名 | ACTA PETROLOGICA SINICA |
2010-04-01 | |
卷号 | 26期号:4页码:1217-1240 |
关键词 | Nushan Lithospheric Mantle Sr-nd-hf-os Isotope Pge |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | Nushan volcano, located in Anhui Province, contains abundant and various mantle-derived peridotitic xenoliths, including spinel lherzolite, garnet lherzolite and spinel-garnet lherzolite, with minor harzburgite. Some spinel lherzolites contain amphibole, phlogopite and apatite, indicating that they had experienced mantle metasomatism. Petrological, mineralogical and geochemical data of the spinel lherzolites and harzbuigites revealed that the former are fertile and the latter are refractory. Depleted Sr-Nd-Hf isotopic characteristics of the spinel lherzolites indicate that they are typical of oceanic peridotites, rather than of Archean lithospheric mantle. Furthermore, most spinal lherzolites have high (187)Os/(188)Os ratios. Although the lithospheric mantle beneath the Nushan are has been strongly metasomatismed by fluids/melts, the Os isotopes and PGE (Platinum Group Element) data display that the Os isotopic composition of the Nushan peridotites are not significantly affected by later mantle metasomatism processes. All these geochemical data of most spinel lherzolites indicate that the lithospheric mantle beneath Nushan are young (Phanerozoic) additions to the subcontinental lithospheric mantle (SCLM) from the convective asthenospheric mantle. However, one harzburgite has relatively lower (187)Os/(188)Os ratio of 0.1184 and ancient Re-depletion age of 1.5Ga, suggesting existence of some ancient component in the asthenosphere. |
WOS关键词 | SINO-KOREAN CRATON ; MESOZOIC ADAKITIC ROCKS ; LOWER CONTINENTAL-CRUST ; TRACE-ELEMENT ; RE-OS ; ABYSSAL PERIDOTITES ; SPINEL PERIDOTITE ; SOUTH CHINA ; SE CHINA ; CENOZOIC BASALTS |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE CHINA PRESS |
WOS记录号 | WOS:000277950600019 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/72962] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Liu ZhiChao |
作者单位 | 1.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Nanjing Univ, State Key Lab Mineral Deposit Res, Dept Earth Sci, Nanjing 210093, Peoples R China |
推荐引用方式 GB/T 7714 | Liu ZhiChao,Wu FuYuan,Chu ZhuYin,et al. Isotopic compositions of the peridotitic xenoliths from the Nushan area, Anhui Province: Constraints on the age of subcontinental lithospheric mantle beneath the East China[J]. ACTA PETROLOGICA SINICA,2010,26(4):1217-1240. |
APA | Liu ZhiChao,Wu FuYuan,Chu ZhuYin,&Xu XiSheng.(2010).Isotopic compositions of the peridotitic xenoliths from the Nushan area, Anhui Province: Constraints on the age of subcontinental lithospheric mantle beneath the East China.ACTA PETROLOGICA SINICA,26(4),1217-1240. |
MLA | Liu ZhiChao,et al."Isotopic compositions of the peridotitic xenoliths from the Nushan area, Anhui Province: Constraints on the age of subcontinental lithospheric mantle beneath the East China".ACTA PETROLOGICA SINICA 26.4(2010):1217-1240. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论