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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