High silicon self-diffusion coefficient in dry forsterite
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Pure climb creep mechanism drives flow in Earth's lower mantle.How do olivines record magmatic events? Insights from major and trace element zoningViscous anisotropy of textured olivine aggregates: 2. Micromechanical modelSmall effect of water on upper-mantle rheology based on silicon self-diffusion coefficients
P2860
High silicon self-diffusion coefficient in dry forsterite
description
im September 2012 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
@nl
наукова стаття, опублікована у вересні 2012
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name
High silicon self-diffusion coefficient in dry forsterite
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High silicon self-diffusion coefficient in dry forsterite
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type
label
High silicon self-diffusion coefficient in dry forsterite
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High silicon self-diffusion coefficient in dry forsterite
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prefLabel
High silicon self-diffusion coefficient in dry forsterite
@en
High silicon self-diffusion coefficient in dry forsterite
@nl
P2093
P50
P1476
High silicon self-diffusion coefficient in dry forsterite
@en
P2093
Chamathni Hegoda
Daisuke Yamazaki
Michael Wiedenbeck
Svyatoslav Shcheka
P304
P356
10.1016/J.EPSL.2012.06.044
P407
P478
P577
2012-09-01T00:00:00Z