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
刊名American Mineralogist
2020
卷号105期号:3页码:363-374
DOI10.2138/am-2020-7075
URL标识查看原文
语种英语
内容类型期刊论文
源URL[http://ir.gyig.ac.cn/handle/42920512-1/11817]  
专题地球化学研究所_地球内部物质高温高压实验室
作者单位1.Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas 78712, U.S.A
2.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
3.Center for Advanced Radiation Sources, University of Chicago, Chicago, Illinois 60437, U.S.A.
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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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