Fitz Gerald, JohnEggleton, RichardKeeling, John2015-12-100935-1221http://hdl.handle.net/1885/56379Asbestiform antigorite from Rowland Flat near Adelaide in South Australia is shown by scanning and transmission electron microscopy to consist of bundles of [010] fibres. Defects combine with grain boundaries to define flattened fibres from 20 nm to 10 μKeywords: antigorite; conference proceeding; crystal structure; grain boundary; microstructure; mineral property; scanning electron microscopy; transmission electron microscopy; Adelaide; Australia; South Australia Antigorite; Asbestiform; Defect; Microstructure; Modulation; SEM; TEM201010.1127/0935-1221/2010/0022-20452016-02-24