中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Highly heterogeneous Late Mesozoic lithospheric mantle beneath the North China Craton: evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks

文献类型:期刊论文

作者Zhang, HF; Sun, M; Zhou, MF; Fan, WM; Zhou, XH; Zhai, MG
刊名GEOLOGICAL MAGAZINE
出版日期2004
卷号141期号:1页码:55-62
关键词Mesozoic continental lithosphere isotopes heterogeneity silicate melts
ISSN号0016-7568
DOI10.1017/S0016756803008331
文献子类Article
英文摘要The lithospheric mantle beneath the North China Craton changed dramatically in its geophysical and geochemical characteristics from Palaeozoic to Cenozoic times. This study uses samples of Mesozoic basalts and mafic intrusions from the North China Craton to investigate the nature of this mantle in Mesozoic times. Sr-Nd-Pb isotopic data demonstrate that the Late Mesozoic lithospheric mantle was extremely heterogeneous. In the central craton or the Luzhong region, it is slightly Sr-Nd isotopically enriched, beneath the Taihangshan region it has an EM1 character (Sr-87/(86)Sri = 0.7050-0.7066; epsilon(Nd(t)) = -17- -10), and beneath the Luxi-haodong region, it possesses EM2-like characteristics (Sr-87/(86)Sri up to 0.7114). Compositional variation with time is also apparent in the Mesozoic lithospheric mantle. Our data suggest that the old lithospheric mantle was modified during Mesozoic times by a silicic melt, where beneath the Luxi-Jiaodong region it was severely modified, but in the Luzhong and Taihangshan regions the effects were much less marked. The silicic melt may have been the product of partial melting of crustal materials brought into the mantle by the subducted slab during the formation of circum-cratonic orogenic belts. This Mesozoic mantle did not survive for a long time, and was replaced by a Cenozoic mantle with depleted geochemical characteristics.
WOS关键词GEOCHEMISTRY ; CONSTRAINTS ; DESTRUCTION ; EVOLUTION ; BASALTS ; BLOCK ; KEEL
WOS研究方向Geology
语种英语
WOS记录号WOS:000220629700004
出版者CAMBRIDGE UNIV PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/64337]  
专题中国科学院地质与地球物理研究所
通讯作者Zhang, HF
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Lab Lithosphere Tecton Evolut, Beijing 100029, Peoples R China
2.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
推荐引用方式
GB/T 7714
Zhang, HF,Sun, M,Zhou, MF,et al. Highly heterogeneous Late Mesozoic lithospheric mantle beneath the North China Craton: evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks[J]. GEOLOGICAL MAGAZINE,2004,141(1):55-62.
APA Zhang, HF,Sun, M,Zhou, MF,Fan, WM,Zhou, XH,&Zhai, MG.(2004).Highly heterogeneous Late Mesozoic lithospheric mantle beneath the North China Craton: evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks.GEOLOGICAL MAGAZINE,141(1),55-62.
MLA Zhang, HF,et al."Highly heterogeneous Late Mesozoic lithospheric mantle beneath the North China Craton: evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks".GEOLOGICAL MAGAZINE 141.1(2004):55-62.

入库方式: OAI收割

来源:地质与地球物理研究所

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