“…Chloritisation of smectite is seen in several geological settings, including the hydrothermal alteration of volcaniclastic rocks (e.g., Inoue and Utada, 1991), metamorphism of pelitic rocks (e.g., Jiang and Peacor, 1994), hydrothermal and regional metamorphism of Mg-silicates and glass in basic igneous rocks (Ragnarsdottir et al, 1984;Schiffman and Fridleiffson, 1991;Shau and Peacor, 1992;Robinson et al, 1993;Schiffman and Staudigel, 1995; and Robinson, 1997) and the hydrothermal alteration of mafic minerals in amphibolites and gneisses (Beaufort and Meunier, 1994). Chloritisation of smectite in late-stage diagenetic to early-stage metamorphic systems may involve the progressive conversion of trioctahedral smectite to chlorite (often via corrensite, Merriman and Peacor, 1999).…”