- journal_title：American Mineralogist
- Contributor：Gian Carlo Capitani ; Marcello Mellini
- Publisher：Mineralogical Society of America
- Date：2007-
- Format：text/html
- Language：en
- Identifier：10.2138/am.2007.2188
- journal_abbrev：American Mineralogist
- issn：0003-004X
- volume：92
- issue：1
- firstpage：64
- section：Articles
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.
Transmission electron microscopy (TEM) of antigorite polysomes with m ranging from 15 to 18 is successfully interpreted on the base of previous X-ray data. In particular, [001] selected area electron diffraction (SAED) patterns show primitive or C-centered cells, for m = 2n or 2n + 1, respectively. In addition, [001] high-resolution (HR) images show 8-reversals aligned or offset by b/2 (i.e., stacking based on a primitive or C-centered lattice).