“…Zeolites have been formed from wastes [ 37 , 38 , 39 , 40 , 41 , 42 , 43 , 44 , 45 , 46 ], natural sources such as clay minerals [ 47 , 48 , 49 , 50 , 51 , 52 , 53 , 54 ] or by adding zeolite seeds in starting gel with or without organic templates [ 55 , 56 , 57 , 58 ]. Recently, natural cost-effective and green silica precursors such as diatomite and obsidian were also used [ 59 , 60 , 61 , 62 , 63 , 64 , 65 , 66 ]. Both materials are interesting natural precursors due to their relatively low cost and highly reactivity although the formation of zeolite type strongly depends on the elemental composition of these natural sources as well as on the used process.…”