TILTING AND DISTORTION OF CASNO3 PEROVSKITE TO 7 GPA DETERMINED FROM SINGLE-CRYSTAL X-RAY DIFFRACTION

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dc.contributor.author Zhao J.
dc.contributor.author Ross N.L.
dc.contributor.author Angel R.J.
dc.date.accessioned 2022-10-31T00:38:52Z
dc.date.available 2022-10-31T00:38:52Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=6620723
dc.identifier.citation Physics and Chemistry of Minerals, 2004, 31, 5, 299-305
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/39299
dc.description.abstract The structural changes of CaSnO3, a GdFeO3-type perovskite, have been investigated to 7 GPa in a diamond-anvil cell at room temperature using single-crystal X-ray diffraction. Significant changes are observed in both the octahedral Sn-O bond lengths and tilt angles between the SnO6 octahedra. The octahedral (SnO6) site shows anisotropic compression and consequently the distortion of SnO6 increases with pressure. Increased pressure also results in a decrease of both of the inter-octahedral angles, ∠Sn-O1-Sn and ∠Sn-O2-Sn, indicating that octahedral tilting increases with increasing pressure, chiefly equivalent to rotation of the SnO6 octahedra about the pseudocubic <001>p axis. The distortion in the CaO12 and SnO6 sites, along with the octahedral SnO6 tilting, is attributed to the SnO6 site being less compressible than the CaO12 site.
dc.subject PEROVSKITE
dc.subject X-RAY DIFFRACTION
dc.subject CRYSTAL STRUCTURE
dc.subject HIGH PRESSURE
dc.title TILTING AND DISTORTION OF CASNO3 PEROVSKITE TO 7 GPA DETERMINED FROM SINGLE-CRYSTAL X-RAY DIFFRACTION
dc.type Статья


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