HIGH-PRESSURE OPTICAL SPECTROSCOPY AND X-RAY DIFFRACTION STUDIES ON SYNTHETIC COBALT ALUMINUM SILICATE GARNET

dc.contributor.authorTaran M.N.
dc.contributor.authorNestola F.
dc.contributor.authorOhashi H.
dc.contributor.authorKoch-Müller M.
dc.contributor.authorBalic-Zunic T.
dc.contributor.authorOlsen L.A.
dc.date.accessioned2026-02-22T07:19:46Z
dc.date.issued2007
dc.description.abstractThe pressure-induced behavior of spin-allowed dd-bands of VIIICo2+ in the absorption spectra of synthetic CO3Al2Si3O12 garnet was studied from 10-4 to 13 GPa. The plots of the peak energy vs. pressure for the three sharpest well resolved bands at ca. 5160, 17 680, and 18 740 cm-1 display small but discernible breaks in linear relations between 4 and 5 GPa. Data from single-crystal X-ray diffraction likewise show discontinuities in trends of CoO8 polyhedral volume and distortion, and Co-O and Si-O bond distances over this pressure range. These effects are related to a pressure-induced phase transition from the β- to α-isostructural polymorph of CO3Al2Si3O12.
dc.identifierhttps://elibrary.ru/item.asp?id=27791137
dc.identifier.citationAmerican Mineralogist, 2007, 92, 10, 1616-1623
dc.identifier.doi10.2138/am.2007.2457
dc.identifier.issn0003-004X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/51314
dc.subjectCOBALT-BEARING GARNET
dc.subjectHIGH-PRESSURE OPTICAL SPECTROSCOPY
dc.subjectHIGH-PRESSURE X-RAY DIFFRACTION
dc.subjectPHASE TRANSITIONS
dc.titleHIGH-PRESSURE OPTICAL SPECTROSCOPY AND X-RAY DIFFRACTION STUDIES ON SYNTHETIC COBALT ALUMINUM SILICATE GARNET
dc.typeСтатья

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