中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geochemical and geochronological studies of the Alegedayi Ophiolitic Complex and its implication for the evolution of the Chinese Altai

文献类型:期刊论文

作者Wong, Kenny1; Sun, Min1; Zhao, Guochun1; Yuan, Chao2; Xiao, Wenjiao3
刊名GONDWANA RESEARCH
出版日期2010-09-01
卷号18期号:2-3页码:438-454
关键词Altai Central Asian Orogenic Belt Accretion Geochemistry Ophiolitic complex Geochronology
ISSN号1342-937X
DOI10.1016/j.gr.2010.01.010
文献子类Article
英文摘要The Alegedayi Ophiolitic Complex (AOC) was discovered in the northwestern part of Altai, Xinjiang, China. Strips of mafic rocks including gabbro, diabase, pillow basalt and pyroxenite, all deformed, mostly underwent low-grade metamorphism, are intercalated with marine-facies sedimentary strata consisting of shale, siltstone and chert. SHRIMP zircon dating of a metagabbro sample gave an age of 439+/-17 Ma. In terms of whole-rock geochemistry, the AOC is composed of three distinct groups. Whereas the majority has transitional or enriched mid-ocean ridge basalt (T-/E-MORB) affinity, varieties with oceanic island basalt (OIB) and supra-subduction zone (SSZ) affinities were also identified. Our data show that the petrogenesis of this mafic complex involved interaction among depleted mantle, enriched component, recycled sediments, slab-derived fluid, and metasomatized mantle wedge. Taking into account the coeval adakites and high-Mg rocks to the southwest and a slightly older arc to the northeast, we suggest that the AOC reflects an intra-arc spreading event that occurred in response to an early Silurian ridge subduction which had profound effects on the tectonic evolution of the Chinese Altai. (C) 2010 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
WOS关键词ASIAN OROGENIC BELT ; HIGH-FIELD-STRENGTH ; PHANEROZOIC CRUSTAL GROWTH ; BACK-ARC BASIN ; DEPLETED-MANTLE SOURCE ; MIDOCEAN RIDGE BASALT ; SLAB-WINDOW FORMATION ; ONTONG JAVA PLATEAU ; RARE-EARTH-ELEMENTS ; EAST PACIFIC RISE
WOS研究方向Geology
语种英语
WOS记录号WOS:000280672000011
出版者ELSEVIER SCIENCE BV
资助机构Hong Kong RGC(HKU7043/07P) ; Hong Kong RGC(HKU7043/07P) ; National Basic Research Program of China(2007CB411308) ; National Basic Research Program of China(2007CB411308) ; GAES of Germany(G-HK030/07) ; GAES of Germany(G-HK030/07) ; Hong Kong RGC(HKU7043/07P) ; Hong Kong RGC(HKU7043/07P) ; National Basic Research Program of China(2007CB411308) ; National Basic Research Program of China(2007CB411308) ; GAES of Germany(G-HK030/07) ; GAES of Germany(G-HK030/07) ; Hong Kong RGC(HKU7043/07P) ; Hong Kong RGC(HKU7043/07P) ; National Basic Research Program of China(2007CB411308) ; National Basic Research Program of China(2007CB411308) ; GAES of Germany(G-HK030/07) ; GAES of Germany(G-HK030/07) ; Hong Kong RGC(HKU7043/07P) ; Hong Kong RGC(HKU7043/07P) ; National Basic Research Program of China(2007CB411308) ; National Basic Research Program of China(2007CB411308) ; GAES of Germany(G-HK030/07) ; GAES of Germany(G-HK030/07)
源URL[http://ir.iggcas.ac.cn/handle/132A11/72606]  
专题中国科学院地质与地球物理研究所
通讯作者Sun, Min
作者单位1.Univ Hong Kong, Dept Earth Sci, Pokfulam, Hong Kong, Peoples R China
2.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Isotope Geochronol & Geochem, Guangzhou 510640, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
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Wong, Kenny,Sun, Min,Zhao, Guochun,et al. Geochemical and geochronological studies of the Alegedayi Ophiolitic Complex and its implication for the evolution of the Chinese Altai[J]. GONDWANA RESEARCH,2010,18(2-3):438-454.
APA Wong, Kenny,Sun, Min,Zhao, Guochun,Yuan, Chao,&Xiao, Wenjiao.(2010).Geochemical and geochronological studies of the Alegedayi Ophiolitic Complex and its implication for the evolution of the Chinese Altai.GONDWANA RESEARCH,18(2-3),438-454.
MLA Wong, Kenny,et al."Geochemical and geochronological studies of the Alegedayi Ophiolitic Complex and its implication for the evolution of the Chinese Altai".GONDWANA RESEARCH 18.2-3(2010):438-454.

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来源:地质与地球物理研究所

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