Magma underplating and Hannuoba present crust-mantle transitional zone composition: Xenolith petrological and geochemical evidence
文献类型:期刊论文
作者 | Fan, QC; Zhang, HF; Sui, JL; Zhai, MG; Sun, Q; Li, N |
刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
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出版日期 | 2005-08-01 |
卷号 | 48期号:8页码:1089-1105 |
关键词 | Magma Underplating Xenolith Petrology Geochemistry Cust-mantle Boundary Constituent Hammoba |
ISSN号 | 1006-9313 |
DOI | 10.1360/04yd0007 |
文献子类 | Article |
英文摘要 | On the basis of mineral assemblage, mineralogy, petrology, and major, trace elemental and isotopic geochemistry of the underplated granulite- and eclogite-facies accumulate, peridotite and pyroxenite xenoliths entrained in Hannuoba Cenozoic basalts, this work constrained the petrological constituents for the crust-mantle transitional zone, which is supported by the results of high-temperature and pressure velocity experiments on rocks and geophysics deep survey. Present lower part of lower crust is mainly composed of granulite-facies mafic accumulates (dominantly plagioclase websterite) and crust-mantle transitional zone dominantly composed of eclogite-facies pyroxenites with or without garnet and spinel lherzolites; Archaean terrain granulite is only nominally early lower crust. Magma underplating in the crust-mantle boundary led to the crustal vertical accretion and the formation of the crust-mantle transitional zone, which is a significant mechanism for the chemical adjustment of the crust-mantle boundary since the Phanerozoic. |
WOS关键词 | NORTH CHINA CRATON ; EASTERN CHINA ; ULTRAMAFIC XENOLITHS ; CONTINENTAL-CRUST ; VOLCANIC-ROCKS ; BOUNDARY ; BENEATH ; LITHOSPHERE ; COMPONENTS ; CHEMISTRY |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000232363900001 |
出版者 | SCIENCE PRESS |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/65524] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Fan, QC |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.China Seismol Bur, Inst Geol, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Fan, QC,Zhang, HF,Sui, JL,et al. Magma underplating and Hannuoba present crust-mantle transitional zone composition: Xenolith petrological and geochemical evidence[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2005,48(8):1089-1105. |
APA | Fan, QC,Zhang, HF,Sui, JL,Zhai, MG,Sun, Q,&Li, N.(2005).Magma underplating and Hannuoba present crust-mantle transitional zone composition: Xenolith petrological and geochemical evidence.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,48(8),1089-1105. |
MLA | Fan, QC,et al."Magma underplating and Hannuoba present crust-mantle transitional zone composition: Xenolith petrological and geochemical evidence".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 48.8(2005):1089-1105. |
入库方式: OAI收割
来源:地质与地球物理研究所
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