中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Lithium isotopic systematics of peridotite xenoliths from Hannuoba, North China Craton: Implications for melt-rock interaction in the considerably thinned lithospheric mantle

文献类型:期刊论文

作者Tang, Yan-Jie; Zhang, Hong-Fu; Nakamura, Eizo; Moriguti, Takuya; Kobayashi, Katsura; Ying, Ji-Feng
刊名GEOCHIMICA ET COSMOCHIMICA ACTA
出版日期2007-09-01
卷号71期号:17页码:4327-4341
ISSN号0016-7037
DOI10.1016/j.gca.2007.07.006
文献子类Article
英文摘要Li concentrations and isotopic compositions of coexisting minerals (ol, opx, and cpx) from peridotite xenoliths entrained in the Hannuoba Tertiary basalts, North China Craton, provide insight into Li isotopic fractionation between mantle minerals during melt-rock interaction in the considerably thinned lithospheric mantle. Bulk analyses of mineral separates show significant enrichment of Li in cpx (2.4-3.6 ppm) relative to olivine (1.2-1.8 ppm), indicating that these peridotites have been affected by mantle metasomatism with mafic silicate melts. Bulk olivine separates (delta Li-7 similar to +3.3 parts per thousand to +6.4 parts per thousand) are isotopically heavier than coexisting pyroxenes (delta Li-7 similar to -3.3 parts per thousand to -8.2 parts per thousand in cpx, and -4.0 parts per thousand to -6.7 parts per thousand in opx). Such large variation suggests Li elemental and isotopic disequilibrium. This conclusion is supported by results from in situ SIMS analyses of mineral grains where significant Li elemental and isotopic zonations exist. The olivine and opx have lower Li concentrations and heavier Li isotopes in the rims than in the cores. This reverse correlation of delta Li-7 with Li concentrations indicates diffusive fractionation of Li isotopes. However, the zoning patterns in coexisting cpx show isotopically heavier rims with higher Li abundances. This positive correlation between delta Li-7 and Li concentrations suggests a melt mixing trend. We attribute Li concentration and isotope zonation in minerals to the effects of two-stage diffusive fractionation coupled with melt-rock interaction. The earliest melts may have been derived from the subducted oceanic slab with low delta Li-7 values produced by isotopic fractionation during the dehydration of the seawater-altered slab. Melts at later stages were derived from the astheno-sphere and interacted with the peridotites, producing the Li elemental and isotopic zoning in mineral grains. These data thus provide evidence for multiple-stage peridotite-melt interaction in the lithospheric mantle beneath the northern North China Craton. (C) 2007 Elsevier Ltd. All rights reserved.
WOS关键词SINO-KOREAN CRATON ; SLAB-DERIVED FLUIDS ; VOLCANIC ARC LAVAS ; CONTINENTAL-CRUST ; MESOZOIC BASALTS ; EASTERN CHINA ; OCEANIC-CRUST ; SUBARC MANTLE ; ICP-MS ; FRACTIONATION
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000249365000014
出版者PERGAMON-ELSEVIER SCIENCE LTD
源URL[http://ir.iggcas.ac.cn/handle/132A11/67200]  
专题中国科学院地质与地球物理研究所
通讯作者Tang, Yan-Jie
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evol, Beijing 100029, Peoples R China
2.Okayama Univ, Inst Study Earths Interior, Pheasant Mem Lab Geochem & Cosmochem, Tottori 6820193, Japan
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GB/T 7714
Tang, Yan-Jie,Zhang, Hong-Fu,Nakamura, Eizo,et al. Lithium isotopic systematics of peridotite xenoliths from Hannuoba, North China Craton: Implications for melt-rock interaction in the considerably thinned lithospheric mantle[J]. GEOCHIMICA ET COSMOCHIMICA ACTA,2007,71(17):4327-4341.
APA Tang, Yan-Jie,Zhang, Hong-Fu,Nakamura, Eizo,Moriguti, Takuya,Kobayashi, Katsura,&Ying, Ji-Feng.(2007).Lithium isotopic systematics of peridotite xenoliths from Hannuoba, North China Craton: Implications for melt-rock interaction in the considerably thinned lithospheric mantle.GEOCHIMICA ET COSMOCHIMICA ACTA,71(17),4327-4341.
MLA Tang, Yan-Jie,et al."Lithium isotopic systematics of peridotite xenoliths from Hannuoba, North China Craton: Implications for melt-rock interaction in the considerably thinned lithospheric mantle".GEOCHIMICA ET COSMOCHIMICA ACTA 71.17(2007):4327-4341.

入库方式: OAI收割

来源:地质与地球物理研究所

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