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Differentiation by Deformation Revisited
Nick Petford, John Clemens
Office of Vice Chancellor
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Keyphrases
Magma
100%
Mush
50%
Crystallization
50%
Compaction
50%
Fractional Crystallization
50%
Hydraulics
25%
Melt Flow
25%
Quantitative Model
25%
Shear Zone
25%
Rheological Properties
25%
Melt Fraction
25%
Igneous Rocks
25%
Resorption
25%
Buoyancy Force
25%
Chemical Constituents
25%
Shear-induced
25%
Shear Modulus
25%
Compositional Changes
25%
Poroelastic Properties
25%
Causes of Variation
25%
Critical Links
25%
Volume Increase
25%
Strain Rate
25%
Granite Differentiation
25%
Liquid Phase
25%
Reverse Zoning
25%
Shear Deformation
25%
Tectonic Background
25%
Contact Geometry
25%
Dilation Angle
25%
Alkaline Rocks
25%
Melt Pressure
25%
Post-failure
25%
Failure Instability
25%
Internal Friction
25%
Phase Petrology
25%
Aplite
25%
Granophyre
25%
Mother Liquor
25%
Pegmatite
25%
Suction Effect
25%
Deformation Potential
25%
Gravitational Effects
25%
Dilatancy Effect
25%
Interstitial Fluid
25%
Miarolitic
25%
Contact Mechanics
25%
Engineering
Late Stage
100%
Driving Force
50%
Hydraulics
50%
Melt Flow
50%
Key Parameter
50%
Liquid Phase
50%
Buoyancy Force
50%
Internal Friction
50%
Shear Modulus
50%
Strain Rate
50%
Contact Mechanics
50%
Chemical Component
50%
Shear Zone
50%
Mother Liquor
50%
Melt Pressure
50%
Resorption
50%
Dilatancy
50%
Shear Deformation
50%
Material Science
Mechanical Strength
100%
Hydraulics
100%
Crystalline Material
100%
Elastic Moduli
100%
Internal Friction
100%
Strain Rate
100%
Igneous Rock
100%
Contact Mechanics
100%
Earth and Planetary Sciences
Magma
100%
Fractional Crystallization
50%
Strain Rate
25%
Petrography
25%
Tectonics
25%
Igneous Rock
25%
Shear Zone
25%
Resorption
25%
Shear Modulus
25%
Internal Friction
25%
Gravitational Effect
25%
Granophyre
25%
Alkaline Rock
25%
Dilatancy
25%
Aplite
25%
Liquid Phase
25%