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Dike ascent in partially molten rock
Allan M. Rubin
Geosciences
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peer-review
95
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Engineering
Compressive Stress
100%
Source Region
100%
Porosity
100%
Observables
50%
Compressibility
50%
Channel Flow
50%
Mass Balance
50%
Crack Growth
50%
Pore Fluid
50%
Host Rock
50%
Field Observation
50%
Fracture Criterion
50%
Crack Initiation
50%
Melt Pressure
50%
Melting Point
50%
Earth and Planetary Sciences
Magma
100%
Pore Pressure
66%
Porosity
66%
Lithosphere
33%
Compressibility
33%
Channel Flow
33%
Peridotite
33%
Host Rock
33%
Crack Initiation
33%
Mechanics
33%
Keyphrases
Dike
100%
Partially Molten Rock
100%
Source Area
14%
Pore Pressure
14%
Compressive Stress
14%
Magma
14%
Porous Flow
14%
Viscous Deformation
14%
Crystallization
7%
Sill
7%
Channel Flow
7%
Buoyancy
7%
Pore Volume
7%
Relevant Parameters
7%
Self-similar Solutions
7%
Pore Fluid
7%
Volume Increase
7%
Mass Balance
7%
Host Rock
7%
Magma Source
7%
Partially Molten
7%
Wetting Angle
7%
Channel Thickness
7%
Peridotite
7%
Subcritical Crack Growth
7%
Griffith Fracture Criterion
7%
Melt Pressure
7%
Melt Reaction
7%
Crack Initiation
7%
Poroelastic
7%
Elastic Compressibility
7%
Conductively Cooled
7%
Rhyolitic
7%