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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

文献类型:期刊论文

作者Dawei Fan; Suyu Fu; Chang Lu; Jingui Xu; Yanyao Zhang; Sergey N. Tkachev; Vitali B. Prakapenka; Jung-Fu Lin
刊名American Mineralogist
出版日期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
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.Center for Advanced Radiation Sources, University of Chicago, Chicago, Illinois 60437, U.S.A.
3.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
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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.

入库方式: OAI收割

来源:地球化学研究所

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