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Garnet-clinopyroxene geothermometer
Authors:S. K. Saxena
Affiliation:1. Department of Geology, Brooklyn College, CUNY, 11210, Brooklyn, New York, USA
Abstract:
A garnet-clinopyroxene geothermometer based on the available experimental data on compositions of coexisting phases in the system MgO-FeO-MnO-Al2O3-Na2O-SiO2 is as follows: $$T({text{}}K) = frac{{8288 + 0.0276 P {text{(bar)}} + Q1 - Q2}}{{1.987 ln K_{text{D}} + 2.4083}}$$ where P is pressure, and Q1, Q2, and K D are given by the following equations $$Q1 = 2,710{text{(}}X_{{text{Fe}}} - X_{{text{Mg}}} {text{)}} + 3,150{text{ }}X_{{text{Ca}}} + 2,600{text{ }}X_{{text{Mn}}} $$ (mole fractions in garnet) $$begin{gathered}Q2 = - 6,594[X_{{text{Fe}}} {text{(}}X_{{text{Fe}}} - 2X_{{text{Mg}}} {text{)]}} hfill {text{ }} - 12762{text{ [}}X_{{text{Fe}}} - X_{{text{Mg}}} (1 - X_{{text{Fe}}} {text{)]}} hfill {text{ }} - 11,281[X_{{text{Ca}}} (1 - X_{{text{Al}}} ) - 2X_{{text{Mg}}} 2X_{{text{Ca}}} ] hfill {text{ + 6137[}}X_{{text{Ca}}} (2X_{{text{Mg}}} + X_{{text{Al}}} )] hfill {text{ + 35,791[}}X_{{text{Al}}} (1 - 2X_{{text{Mg}}} )] hfill {text{ + 25,409[(}}X_{{text{Ca}}} )^2 ] - 55,137[X_{{text{Ca}}} (X_{{text{Mg}}} - X_{{text{Fe}}} )] hfill {text{ }} - 11,338[X_{{text{Al}}} (X_{{text{Fe}}} - X_{{text{Mg}}} )] hfill end{gathered} $$ [mole fractions in clinopyroxene Mg = MgSiO3, Fe = FeSiO3, Ca = CaSiO3, Al = (Al2O3-Na2O)] K D = (Fe/Mg) in garnet/(Fe/Mg) in clinopyroxene. Mn and Cr in clinopyroxene, when present in small concentrations are added to Fe and Al respectively. Fe is total Fe2++Fe3+.
Keywords:
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