“…introduction Diffusion-induced mineral zonation is an important phenomenon in metasomatic processes (processes involving changes in the chemical composition of rock), causing replacement of an initial suite of minerals in a permeable medium with one or more regions of different mineral combinations. Systems such as the dissolution of hydroxyapatite (Kim and Cussler, 1987) have been experimentally examined, and some geochemical systems have been analyzed mathematically (Cussler et al, 1983;Lichtner et al, 1986 a, b;Kopinsky et al, 1988). While the convection-dominated analog to this problem has been studied extensively (Bryant, 1986;Bryant et al, 1986Bryant et al, , 1987Dria, 1988;Lichtner, 1985;Schechter et al, 1987;Walsh, 1983;Walsh et al, 1982Walsh et al, , 1984, the diffusion-only regime has not received the same rigorous treatment.…”