“…A number of authors have recorded veinlets and veins of apophyllite in different rocks, for example, with zeolites and calcite in the gneisses of the Aar massif (Konigsberger, 1901); in rapakivi granites and their pegma tites in Finland and the Ukraine ( Fersman, 1952;Volborth, 1953;Vorma, 1961;Nazarenko, 1963;Litvin et al, 1964); along with natrolite in aegirine-hornblende nepheline syenites and pegmatites (Barabanov, 1957(Barabanov, , 1960; with zeolites, quartz, and calcite in basalts in Nova Scotia, Canada (Walker and Parsons, 1922); with calcite and zeolites, in the Eocene volcanic rocks of Georgia (Gvakhariya, 1951); in the Siberian traps (Cherepanov and Murina, 1966) ; with calcite, celadonite, earlier quartz, mesolite, natrolite, chalcedony, and datolite, in the volcanic rocks of the Karadag in the Crimea (Suprychev, 1968); with quartz and prehnite, in the leucocratic quartz gabbros in northern Kazakhstan (Spiridonov, 1964); with calcite and prehnite, in leaching cavities among the olivine gabbro-norites of Noril'sk (Vasil'yev, 1968); with zeolites and calcite, in the non-ore skarns of the Chatkal region (Yenikeyev and Prikhod'ko, 1949;Povarennykh, 1952) ; in the non-ore skarns of the southeastern Standzha-Planina in Bulgaria (Kostov, 1962) ; and with prehnite, in a garnetdiopside rock at Crestmore in California (Bailey, 1941). In Hintze's handbook ( 1896), data are also given on the occurrence of apo phyllite in prehnite-bearing veins among wollastonite rocks in Hessen, and in a number of places in Romania, in veins among gneisses in Saxony (with quartz and calcite), in amygdules of effusive rocks and in the veinlets cut ting them in many regions.…”