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X-ray diffraction evidence for a monoclinic form of stibnite, [Sb.sub.2][S.sub.3], below 290 K
- Source :
- American Mineralogist. July, 2004, Vol. 89 Issue 7, p1022, 4 p.
- Publication Year :
- 2004
-
Abstract
- The nature of the symmetry changes associated with phase transitions in stibnite, [Sb.sub.2][S.sub.3], has been investigated by powder and single crystal X-ray diffraction. Above 420 K stibnite (I) is centrosymmetric Pbnm. Stibnite (II) is stable between 290 and 420 K and is acentric [P2.sub.1]nm. Below 290 K stibnite (III) is stable and systematic absences indicates that this phase is monoclinic with space group [P2.sub.1] or Pm, or triclinic P1, but the cell dimensions remain geometrically orthorhombic. These findings are in agreement with variations in physical and electrical properties reported in the literature.
- Subjects :
- Mineralogy -- Research
Earth sciences
Subjects
Details
- Language :
- English
- ISSN :
- 0003004X
- Volume :
- 89
- Issue :
- 7
- Database :
- Gale General OneFile
- Journal :
- American Mineralogist
- Publication Type :
- Academic Journal
- Accession number :
- edsgcl.120102848