Work on two sheet organosilicon polymers, one derived from the mineral chrysotile and the other from the mineral apophyllite, is described. This work provides direct evidence that both these polymers are composed of sheets. In addition, it shows that in the chrysotile‐derived polymer the sheets curl into scrolls, and that in the apophyllite‐derived polymer the sheets are essentially flat.
Chlorophthalocyaninato‐aluminium (Ia) wurde nach einer modifizierten Literaturmethode durch 30 min Rückflußkochen einer Mischung aus Phthalonitril, AlCl3 und Chinolin dargestellt.
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