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Phase Equilibria Involving Nonideal Solutions and Outlines of Geothermometry and Geobarometry,ct the condition of equilibrium. The extraction of the temperature of equilibration is geothermometry; geobarometry is the calculation of the pressure of equilibrium for any assemblage. Because the T and P of solid-solid reactions are independent of the activity or fugacity of fluids prevalent durin
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as helped put mineralogy and petrology on a firm quantitative basis. In the wake of these developments, academic curricula now require the students of geology to take a course in basic thermodynamics, traditionally offered by the departments of chemistry. Building on that foundation, a supplementary course is978-3-540-53215-6978-3-662-02716-5
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