Shaw, Cliff S. J. (2004) Mechanisms and rates of quartz dissolution in melts in the CMAS (CaO?MgO?Al2O3?SiO2) system. Contributions to Mineralogy and Petrology, 148 (2) 180-200 doi:10.1007/s00410-004-0581-3

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See Also

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	Shaw, Cliff S. J. (2006) Effects of melt viscosity and silica activity on the rate and mechanism of quartz dissolution in melts of the CMAS and CAS systems. Contributions to Mineralogy and Petrology, 151 (6) 665-680 doi:10.1007/s00410-006-0086-3
	Shaw, Cliff S. J. (2012) The effects of potassium addition on the rate of quartz dissolution in the CMAS and CAS systems. Contributions to Mineralogy and Petrology, 164 (5) 839-857 doi:10.1007/s00410-012-0777-x
	Heinrich, Wilhelm, Churakov, Sergey S., Gottschalk, Matthias (2004) Mineral-fluid equilibria in the system CaO?MgO?SiO2?H2O?CO2?NaCl and the record of reactive fluid flow in contact metamorphic aureoles. Contributions to Mineralogy and Petrology, 148 (2) 131-149 doi:10.1007/s00410-004-0598-7
	Hensen, B. J., Essene, E. J. (1971) Stability of pyrope-quartz in the system MgO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 30 (1) 72-83 doi:10.1007/bf00373370
	Gardés, E., Heinrich, W. (2011) Growth of multilayered polycrystalline reaction rims in the MgO–SiO2 system, part II: modelling. Contributions to Mineralogy and Petrology, 162 (1) 37-49 doi:10.1007/s00410-010-0581-4
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	Nickel, K. G., Brey, G. P., Kogarko, L. (1985) Orthopyroxene-clinopyroxene equilibria in the system CaO-MgO-Al2O3-SiO2 (CMAS): new experimental results and implications for two-pyroxene thermometry. Contributions to Mineralogy and Petrology, 91 (1) 44-53 doi:10.1007/bf00429426
	Hermann, J., O’Neill, H. S. C., Berry, A. J. (2005) Titanium solubility in olivine in the system TiO2–MgO–SiO2: no evidence for an ultra-deep origin of Ti-bearing olivine. Contributions to Mineralogy and Petrology, 148 (6) 746-760 doi:10.1007/s00410-004-0637-4
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	Brey, G. P., Nickel, K. G., Kogarko, L. (1986) Garnet-pyroxene equilibria in the system CaO-MgO-Al2O3-SiO2 (CMAS): prospects for simplified (?T-independent?) lherzolite barometry and an eclogite-barometer. Contributions to Mineralogy and Petrology, 92 (4) 448-455 doi:10.1007/bf00374427