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Single-crystal structure determinations of the m = 17 and m = 16 antigorite polysomes confirmed the existence of two basic antigorite structures, i.e., “odd” antigorites, with m = 2n + 1 (m being the number of tetrahedra in a wavelength visible in the [010] projections), and “even” antigorites, with m = 2n. Both structures contain .8-reversals. and “6-reversals”. The “8-reversals” consist of 8-member rings of tetrahedra, where four tetrahedra point in one direction and four in the opposite direction, whereas “6-reversals” involve four tetrahedra and two tetrahedra, respectively. “Odd” antigorites have m tetrahedra and m − 1 octahedra along a wavelength (which coincides with the a translation) and Pm space group. Conversely, b/2 shifts every second 8-reversal cause the structure to be C-centered in “even” antigorites (C2/m space group). In the latter case, m tetrahedra and m − 1 octahedra occur within a wave, but two waves occur within an a periodicity.

High-resolution transmission electron microscopy (HRTEM) investigation of antigorite polysomes (m = 15 to 18)