T-XCO2 stability relations and phase equilibria of a calcic carbonate scapolite

At a total pressure of 5 kb, calcic, Cl-free scapolite (Me₈₃) is stable relative to plagioclase-bearing assemblages at $\text{T ≧ 625°C}$, . With decreasing temperature, scapolite breaks down to plagioclase + calcite. Scapolite is replaced by plagioclase + grossular + cancrinite + CO₂ in the presence of H₂O-rich fluids. The stable coexistence of scapolite and calcite, an assemblage typical of most natural occurrences of calcic scapolite, is limited by the reaction: scapolite + calcite → grossular + cancrinite + CO₂, which occurs at 750°C, X_CO2 = 0.46; 700°C, X_CO2 = 0.33; 650°C, X_CO2 = 0.18, for the chosen bulk composition.Generalization of the experimental results to encompass the complete range of fully carbonated scapolite compositions indicates that mizzonite (Me₇₅) has the largest T-X_CO2 stability field. For scapolite more calcic than mizzonite, stable growth is restricted to conditions of increasingly higher temperature and X_CO2.The experimental results are consistent with various petrologic features of scapolite-bearing rocks, particularly scapolite-clinopyroxene granulites, and indicate that such rocks were formed in the presence of CO₂-rich fluids.