Natural zeolites filling amygdales and veins in basalts from the British Tertiary Igneous Province on the Isle of Skye, Scotland

natural zeolites filling amygdales and veins in tertiary basaltic host rocks on the isle of skye (nw scotland) have been studied in some detail by transmitted light microscopy, scanning electron microscopy and x-ray diffraction techniques. the zeolites and associated minerals so identified in order of their relative time of formation from early to late were nontronite, amorphous silica phases, carbonate phases, chabazite, phillipsite, wairakite, thomsonite, analcime, natrolite and stilbite-type minerals. zeolite formation in the skye basalts began with low si/al ratio na zeolites and a gradual increase in ca content and si/al ratio, ending up as ca zeolites. they were probably formed as a consequence of late-stage hydrothermal activity, although, locally, contact metamorphism may control the process of zeolite formation