Metamorphic Reactions
Phase Transformation Reactions
Solid-Solid Net Transfer Reaction NaAlSi 2 O 6 + SiO 2 = NaAlSi 3 O 8 Jd QtzAb dG = VdP – SdT dP = S dT = V Clapyron Equation
Dehydration Reaction KAl 3 Si 3 O 10 (OH) 2 + SiO 2 = KAlSi 3 O 8 + Al 2 SiO 5 + H 2 O Ms Qtz Kfs Als Slope of reaction boundary determined by properties of fluid phase dP = S dT = V Most dehydration reaction boundaries subparallel
Decarbonation Reactions CaCO 3 + SiO 2 = CaSiO 3 + CO 2 Parallelism of decarbonation reaction equilibrium boundaries in P-T space
Decarbonation Versus Dehydration Reactions
Theoretical Loop of Devolatilization Reactions At high enough pressures the fluid phase is so compressed that V Products < V Reactants dP = S dT = V Clapyron equation becomes negative
Dehydration Reaction: Effect of P H 2 O < P Total Ln K = Ln f H 2 O ( f H 2 O = P H 2 O H 2 O ) Le Chatelier’s principle; lowering PH2OPH2O stabilizes products at the expense of reactants, displacing equilibrium boundary to lower temperature
Temperature vs Mole Fraction of Fluid Species T-X H 2 O Diagram T-X CO 2 Diagram X CO 2 + X H 2 O = 1
G T G T K A S G T A K S K S A T P3 P2 P1 P3 P2 P1 T (K) (A) (S) Energy-Temperature Diagrams: the Rules of Schreinemakers P1 P3 P2
Rules of Schreinemakers 1.Label each reaction with the missing phase 2.Arrange reactions such that the label is stable where the reaction is metastable
Application of Rules of Schreinemakers to 2-component system with 4 phases Note that there is one reaction for each phase in the system
Application of Rules of Schreinemakers to 2-Component System with 5 phases
An Example of a Petrogenetic Grid – the KMASH System for Pelites