中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Metasomatism of mesozoic and cenozoic lithospheric mantle beneath the north china craton: Evidence from phlogopite-bearing mantle xenoliths

文献类型:期刊论文

作者Zhao, X. M.; Zhang, H. F.; Zhu, X. K.; Zhang, W. H.; Yang, Y. H.; Tang, Y. J.
刊名ACTA PETROLOGICA SINICA
出版日期2007-06-01
卷号23期号:6页码:1281-1293
关键词cenozoic basalt phlogopite-bearing mantle xenolith mantle metasomatism lithospheric mantle north china craton
ISSN号1000-0569
文献子类Article
英文摘要This paper reports the mineral compositions, clinopyroxene trace element concentrations and Sr-Nd isotopes for the newly-discovered phlogopite-bearing spinel lherzolite and olivine clinopyroxenite xenoliths from three different localities ( Hannuoba, Hebei Province; Jining Sanyitang, Inner Mongolia; Hebi, Henan Province) of the North China Craton. Systematic comparison with those phlogopite-free spinel lherzolite xenoliths from the same localities reveals that the pblogopite-bearing peridotitic xenoliths have relatively higher Al2O3, CaO, Na2O, K2O, TiO2 contents and lower MgO contents than those phlogopite-free counterparts. The former also has higher LREE concentrations, but relatively less radiogenic Sr-Nd isotopic ratios. This demonstrates that mantle metasomatism can not only enrich the basaltic components and trace element concentrations, but also make a decrease in Mg-# of the peridotites and olivines and a relative depletion in Sr-Nd isotopes. Rb-87/Sr-86-Sr-87/(86) Sr isochrons of the phlogopite-bearing xenoliths indicate that mantle metasomatism happened in the Mesozoic and/or Cenozoic time. The metasomatic agent was derived from the asthenosphere. The result also manifests that the widespread similarity of the geochemical features such as major and trace elements and isotopic compositions in the Cenozoic lithospheric mantle beneath the North China Craton to those "oceanic" lithospheric mantle could be as a result of the ubiquitous presence of the interaction between the old refractory peridotites and the infiltrated asthenospheric melt, rather than the actually newly-accreted lithospheric mantle.
WOS关键词SINO-KOREAN CRATON ; PYROXENITE XENOLITHS ; PERIDOTITE XENOLITHS ; INNER-MONGOLIA ; EASTERN CHINA ; TRACE-ELEMENT ; GEOCHEMISTRY ; HANNUOBA ; ND ; BASALTS
WOS研究方向Geology
语种英语
WOS记录号WOS:000248791900005
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/68420]  
专题中国科学院地质与地球物理研究所
通讯作者Zhao, X. M.
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Chinese Acad Geol Sci, Inst Geol, Key Lab Isotop Geol Minist Land & Resources, Beijing 100037, Peoples R China
推荐引用方式
GB/T 7714
Zhao, X. M.,Zhang, H. F.,Zhu, X. K.,et al. Metasomatism of mesozoic and cenozoic lithospheric mantle beneath the north china craton: Evidence from phlogopite-bearing mantle xenoliths[J]. ACTA PETROLOGICA SINICA,2007,23(6):1281-1293.
APA Zhao, X. M.,Zhang, H. F.,Zhu, X. K.,Zhang, W. H.,Yang, Y. H.,&Tang, Y. J..(2007).Metasomatism of mesozoic and cenozoic lithospheric mantle beneath the north china craton: Evidence from phlogopite-bearing mantle xenoliths.ACTA PETROLOGICA SINICA,23(6),1281-1293.
MLA Zhao, X. M.,et al."Metasomatism of mesozoic and cenozoic lithospheric mantle beneath the north china craton: Evidence from phlogopite-bearing mantle xenoliths".ACTA PETROLOGICA SINICA 23.6(2007):1281-1293.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

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。