A Chemical and Thermodynamic Model of Aluminous Dioctahedral 2:1 Layer Clay Minerals in Diagenetic Processes; Regular Solution Representation of Interlayer Dehydration in Smectite
Ransom, B., & Helgeson, H. C. (1994). A chemical and thermodynamic model of aluminous dioctahedral 2:1 layer clay minerals in diagenetic processes; regular solution representation of interlayer dehydration in smectite. American Journal of Science, 294(4), 449–484. https://doi.org/10.2475/ajs.294.4.449