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Table 7 Reaction relations without volume constraints

From: Interplay of irreversible reactions and deformation: a case of hydrofracturing in the rodingite–serpentinite system

CaO–SiO2–AF subsystem ∆V
1.00Atg + 12.98Di + 4.28Grt + 3.92FM = 24.21DiRZ + 3.77ChlRZ + 0.83H2O 0.60%
1.00Atg + 3.84Di + 4.11Grt + 2.77FM = 14.86DiRZ + 3.67ChlRZ + 1.67H2O −0.60%
CaO–SiO2–FM subsystem
1.00Atg + 12.67Di + 8.06Grt = 34.16DiRZ + 2.39ChlRZ + 61.38AF + 11.90H2O −70.80%
1.00Atg + 7.14Di + 7.27Grt = 26.65DiRZ + 2.57ChlRZ + 45.34AF + 10.41H2O −61.69%
CaO–AF–FM subsystem
1.00Atg + 9.47Di + 3.81Grt = 19.53DiRZ + 3.49ChlRZ + 2.43SiO2 + 3.07H2O −4.10%
1.00Atg + 1.80Di + 3.77Grt = 11.98DiRZ + 3.47ChlRZ + 1.75SiO2 + 3.24H2O −4.80%
SiO2–AF–FM subsystem
1.00Atg + 7.11Di + 3.59Grt + 1.85CaO = 18.43DiRZ + 3.36ChlRZ + 4.08H2O −2.20%
1.00Atg + 0.34Di + 3.62Grt + 1.35CaO = 11.44DiRZ + 3.38ChlRZ + 3.97H2O −3.10%