THE HIGH-TEMPERATURE P2/C1-C2/C PHASE TRANSITION IN FE-FREE CA-RICH P21/C CLINOPYROXENES

dc.contributor.authorTribaudino M.
dc.contributor.authorNestola F.
dc.contributor.authorMeneghini C.
dc.contributor.authorBromiley G.D.
dc.date.accessioned2022-02-13T04:46:09Z
dc.date.available2022-02-13T04:46:09Z
dc.date.issued2003
dc.description.abstractAn in situ, high-temperature, powder diffraction investigation was performed for iron-free clinopyroxenes with compositions Ca0.40Mg1.60Si2O6, Ca0.52Mg1.46Al0.05Si1.98O6, Ca0.59Mg1.41Si2O6 and Ca0.70Mg1.30Si2O6, up to 850 °C using synchrotron radiation (ESRF, Grenoble). In samples with compositions Ca0.52Mg1.46Al0.05Si1.98O6 and Ca0.59Mg1.41Si2O6, evidence of for the P21/c-C2/c displacive phase transition was seen in changes in lattice parameters at T ≈ 550 and 300 °C respectively. Landau modelling of the phase transition behaviour for the sample with composition Ca0.52Mg1.46Al0.05Si1.98O6 shows a tricritical behaviour [Tc=547(16)]. Comparison with the transition behaviour in other samples with lower Ca contents along the join diopside-enstatite indicates that a decrease in Tc, and a switch from first-order to tricritical behavior occurs with increasing Ca content. The change in the transition behaviour was related to an interaction with the antiphase domains at the nanoscale.
dc.identifierhttps://elibrary.ru/item.asp?id=5108141
dc.identifier.citationPhysics and Chemistry of Minerals, 2003, 30, 9, 527-535
dc.identifier.issn0342-1791
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/35279
dc.subjectCLINOPYROXENE
dc.subjectIN SITU HT POWDER DIFFRACTION
dc.subjectSYNCHROTRON RADIATION
dc.subjectPHASE TRANSITION
dc.subjectTHERMAL EXPANSION
dc.titleTHE HIGH-TEMPERATURE P2/C1-C2/C PHASE TRANSITION IN FE-FREE CA-RICH P21/C CLINOPYROXENES
dc.typeСтатья

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