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When F=1, P + 1 = =3. Thus, the following univariant reactions and assemblages are possible d=c+g d=c+w g=d+w g=c+w
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Predict the possible reactions from the compositions of the phases in a system.
Unary system: C=1. All phases have same composition A “point”. Only phase transition is possible
Binary system: C=2. Phases are on a line.
3. Chemography
A B
1 2 3X
Example: Al2O3-H2O system Possible phases
Corundum Al2O3 (c)Diaspoer AlOOH (d)Gibbsite Al(OH)3 (g)Water H2O (w)
Al2O3 H2O
c wd g
When F=1, P + 1 = 2 + 2 =3. Thus, the following univariant reactions and
assemblages are possibled=c+gd=c+wg=d+wg=c+w
Ternary System: C=3, Phases are on a triangle
A
C
B
2
1
34
5
When F=1, P=3-1+2=4. Two possible univariant reactions;
Phase elimination reaction: 4=1+2+3 Join-crossing reaction: 1+2=3+4
A
C
B A
C
B
42
1
3
1
3
4
2
Example: SiO2-CaO-MgO-(H2O-CO2) system Possible phases
Quartz SiO2 (Qz) Calcite CaCO3 (Cc) Dolomite CaMg(CO3)2 (Dm) Tremolite Ca2Mg5Si8O22(OH)2 (Tr) Diopside CaMgSi2O6 (Dp) Forsterite Mg2SiO4 (Fo) Chondrodite Mg5Si2O8(OH)2 (Cd) Wollastonite CaSiO3 (Ws) Magnesite (MgCO3) (Mg)
With constant fugacities of H2O and CO2
CaO(C) MgO(M)
SiO2(S)
Cc
DmMg
Ws
Qz
Dp Tr
Fo
Cd
Metamorphic mineral reactions as a function of T
Qz+DmTr+Cc Qz+Tr+CcDpOriginal assemblage Cc+TrDi+Dm
Tr+Dm Di+Fo Di+Dm Cc+Fo