Figure 5
Structure of the slices and , both belonging to the [001] zone of aragonite: the {110} prism can show two profiles that are pseudo-symmetrically equivalent, generated from two types of building units (BU1 or BU2), whereas the {010} pinacoid, whose profile should be unique, is built by BU2 only. Note the strong similarity between the and slices. The meaning of the term `building unit' has been described previously elsewhere (Aquilano et al., 1997) and the bonds that make each BU are illustrated in detail. |