“…Mineralogical analyses of initially smectite rich rocks heated to more that 80e100 C has shown that the silica has been precipitated as small quartz crystals which develop into sheets of quartz producing a distinct schistocity (Thyberg et al, 2009(Thyberg et al, , 2010Thyberg and Jahren, 2011). Day-Stirrat et al (2010) found that here is a decrease in the content of quartz, K-feldspar and kaolinite and an increase in illite and smectite with depth.…”