Electrical conductivity during incipient melting in the oceanic low-velocity zone.
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Experimental evidence supports mantle partial melting in the asthenosphereOlivine anisotropy suggests Gutenberg discontinuity is not the base of the lithosphere.Petit-spot as definitive evidence for partial melting in the asthenosphere caused by CO2Ultralow viscosity of carbonate melts at high pressures.Evidence for frozen melts in the mid-lithosphere detected from active-source seismic data.Transport properties of carbonated silicate melt at high pressure.Constraints on volumes and patterns of asthenospheric melt from the space-time distribution of seamountsAbnormal acoustic wave velocities in basaltic and (Fe,Al)-bearing silicate glasses at high pressuresToward a unified hydrous olivine electrical conductivity lawCarbon contents in reduced basalts at graphite saturation: Implications for the degassing of Mars, Mercury, and the Moon
P2860
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P2860
Electrical conductivity during incipient melting in the oceanic low-velocity zone.
description
2014 nî lūn-bûn
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2014年の論文
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2014年学术文章
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2014年学术文章
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2014年学术文章
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2014年学术文章
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2014年学术文章
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2014年學術文章
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2014年學術文章
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2014年學術文章
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name
Electrical conductivity during incipient melting in the oceanic low-velocity zone.
@en
Electrical conductivity during incipient melting in the oceanic low-velocity zone.
@nl
type
label
Electrical conductivity during incipient melting in the oceanic low-velocity zone.
@en
Electrical conductivity during incipient melting in the oceanic low-velocity zone.
@nl
prefLabel
Electrical conductivity during incipient melting in the oceanic low-velocity zone.
@en
Electrical conductivity during incipient melting in the oceanic low-velocity zone.
@nl
P2093
P2860
P356
P1433
P1476
Electrical conductivity during incipient melting in the oceanic low-velocity zone.
@en
P2093
David Sifré
Emmanuel Gardés
Leila Hashim
Malcolm Massuyeau
P2860
P2888
P356
10.1038/NATURE13245
P407
P577
2014-05-01T00:00:00Z
P5875
P6179
1012636272