• journal_title：American Mineralogist
• Contributor：Roman Skála ; Ivana Císařová ; Milan Drábek
• Publisher：Mineralogical Society of America
• Date：2006-
• Format：text/html
• Language：en
• Identifier：10.2138/am.2006.1999
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：91
• issue：5-6
• firstpage：917
• section：Articles

id="p-1">The crystal structure of troilite from chondrites Etter and Georgetown and a troilite analog synthesized by sulfurization of an iron wire was refined using single-crystal X-ray data. Troilite is known to be hexagonal, with space group P6̅2c, which is non-centrosymmetric, allowing two non-identical inversely related spatial arrangements of atoms within the unit cell. All three samples represent the so-called inversion twins. They contain both inversely related atomic orientations instead of a single atomic arrangement. The inversion twinning may have developed as a result of a phase transition from the ideal centrosymmetric NiAs-type structure to troilite-type structure during cooling. In addition, all samples were found to be cation-deficient. The departure from ideal stoichiometry—up to almost 3.5 rel% of metal atoms are missing—is also possibly related to atomic ordering when the crystals cooled.