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Hot Under the Collar (part III) Phase Diagrams
Rocks at last!!!!
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Gibbs Phase Rule F = C - P + 2 F = the number of degrees of freedom
C = the number of components P = number of phases
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Gibbs Phase Rule Divarient Field Point C F = C - P + 2 Only one phase
Only one component (e.g. H2O exists as ice, water and steam but is always present as H2O) Therefore two degrees of freedom Divarient Field
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Gibbs Phase Rule Univarient Line Point B F = C - P + 2 Two phases
Only one component (e.g. H2O exists as ice, water and steam but is always present as H2O) Therefore one degree of freedom Univarient Line
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Gibbs Phase Rule Invarient Point Point A F = C - P + 2 Three phases
Only one component (e.g. H2O exists as ice, water and steam but is always present as H2O) Therefore no degrees of freedom Invarient Point
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Two component phase diagrams – mixtures between two endmembers
Binary Phase Diagrams Two component phase diagrams – mixtures between two endmembers
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Binary Phase Diagrams Eutectic Liquidus Solidus
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Equilibrium BALANCE MgO + SiO MgSiO3 periclase quartz enstatite
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Binary Phase Diagrams
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Binary Phase Diagrams
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Binary Phase Diagrams
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Binary Phase Diagrams
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Lever Rule F = L2/L1 F is the fraction of melt remaining
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Lever Rule F = L3/L1 F is the fraction of crystals of B L3
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Lever Rule F = L2/L1 F is the fraction of crystals of B generated at the eutectic
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Lever Rule F = L2/L1 F is the fraction total fraction of B in the whole rock
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Disequilibrium Reactions are not balanced Rapid cooling
Separation of crystals by sinking or flotation (crystal differentiation) “Protection” of crystals by the formation of rims or zoning.
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At Disequilibrium
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At Disequilibrium
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At Disequilibrium
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At Disequilibrium
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Solid Solutions
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Solid Solutions
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Solid Solutions
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Lever Rule F = L2/L1 F is the fraction of liquid left.
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Under Disequilibrium
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Under Disequilibrium
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Under Disequilibrium
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Why phase diagrams are the way they are!!!!
Next Time Why phase diagrams are the way they are!!!!
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