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Elasticity of single-crystal Fe-enriched diopside at high-pressure conditions: Implications for the origin of upper mantle low-velocity zones
Dawei Fan; Suyu Fu; Chang Lu; Jingui Xu; Yanyao Zhang; Sergey N. Tkachev; Vitali B. Prakapenka; Jung-Fu Lin
2020
Source PublicationAmerican Mineralogist
Volume105Issue:3Pages:363-374
DOI10.2138/am-2020-7075
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Indexed BySCI
Language英语
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Cited Times:8[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/11817
Collection地球内部物质高温高压实验室
Affiliation1.Key Laboratory of High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550081, China
2.Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas 78712, U.S.A
3.Center for Advanced Radiation Sources, University of Chicago, Chicago, Illinois 60437, U.S.A.
Recommended Citation
GB/T 7714
Dawei Fan,Suyu Fu,Chang Lu,et al. Elasticity of single-crystal Fe-enriched diopside at high-pressure conditions: Implications for the origin of upper mantle low-velocity zones[J]. American Mineralogist,2020,105(3):363-374.
APA Dawei Fan.,Suyu Fu.,Chang Lu.,Jingui Xu.,Yanyao Zhang.,...&Jung-Fu Lin.(2020).Elasticity of single-crystal Fe-enriched diopside at high-pressure conditions: Implications for the origin of upper mantle low-velocity zones.American Mineralogist,105(3),363-374.
MLA Dawei Fan,et al."Elasticity of single-crystal Fe-enriched diopside at high-pressure conditions: Implications for the origin of upper mantle low-velocity zones".American Mineralogist 105.3(2020):363-374.
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