GYIG OpenIR  > 地球内部物质高温高压实验室
Temperature-enhanced electrical conductivity anisotropy in partially molten peridotite under shear deformation
Baohua Zhang; Takashi Yoshino
2020
Source PublicationEarth and Planetary Science Letters
Volume530Pages:115922
DOI10.1016/j.epsl.2019.115922
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Indexed BySCI
Language英语
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Cited Times:7[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/11889
Collection地球内部物质高温高压实验室
地球深部物质与流体作用地球化学研究室
Affiliation1.Institute of Geology and Geophysics, School of Earth Sciences, Zhejiang University, Hangzhou 310027, China
2.Key Laboratory for High-Temperature and High-Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550081, China
3.Institute for Planetary Materials, Okayama University, Misasa, Tottori-ken 682-0193, Japan
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GB/T 7714
Baohua Zhang,Takashi Yoshino. Temperature-enhanced electrical conductivity anisotropy in partially molten peridotite under shear deformation[J]. Earth and Planetary Science Letters,2020,530:115922.
APA Baohua Zhang,&Takashi Yoshino.(2020).Temperature-enhanced electrical conductivity anisotropy in partially molten peridotite under shear deformation.Earth and Planetary Science Letters,530,115922.
MLA Baohua Zhang,et al."Temperature-enhanced electrical conductivity anisotropy in partially molten peridotite under shear deformation".Earth and Planetary Science Letters 530(2020):115922.
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