Vol. 295, Issue 3, 1995March 01, 1995 EDT
A Chemical and Thermodynamic Model of Dioctahedral 2:1 Layer Clay Minerals in Diagenetic Processes; Dehydration of Dioctahedral Aluminous Smectite as a Function of Temperature and Depth in Sedimentary Basins
A Chemical and Thermodynamic Model of Dioctahedral 2:1 Layer Clay Minerals in Diagenetic Processes; Dehydration of Dioctahedral Aluminous Smectite as a Function of Temperature and Depth in Sedimentary Basins
Barbara Ransom, Harold C. Helgeson,
Ransom, B., & Helgeson, H. C. (1995). A chemical and thermodynamic model of dioctahedral 2:1 layer clay minerals in diagenetic processes; dehydration of dioctahedral aluminous smectite as a function of temperature and depth in sedimentary basins. American Journal of Science, 295(3), 245–281. https://doi.org/10.2475/ajs.295.3.245