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

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dc.contributor.author Tribaudino M.
dc.contributor.author Nestola F.
dc.contributor.author Meneghini C.
dc.contributor.author Bromiley G.D.
dc.date.accessioned 2022-02-13T04:46:09Z
dc.date.available 2022-02-13T04:46:09Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=5108141
dc.identifier.citation Physics and Chemistry of Minerals, 2003, 30, 9, 527-535
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/35279
dc.description.abstract An 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.subject CLINOPYROXENE
dc.subject IN SITU HT POWDER DIFFRACTION
dc.subject SYNCHROTRON RADIATION
dc.subject PHASE TRANSITION
dc.subject THERMAL EXPANSION
dc.title THE HIGH-TEMPERATURE P2/C1-C2/C PHASE TRANSITION IN FE-FREE CA-RICH P21/C CLINOPYROXENES
dc.type Статья


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