THE P21/M ↔ C2/M PHASE TRANSITION IN SYNTHETIC AMPHIBOLE NA NAMG MG5 SI8 O22 (OH)2: THERMODYNAMIC AND CRYSTAL-CHEMICAL EVALUATION

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dc.contributor.author Cámara F.
dc.contributor.author Oberti R.
dc.contributor.author Iezzi G.
dc.contributor.author Della Ventura G.
dc.date.accessioned 2022-02-17T11:03:56Z
dc.date.available 2022-02-17T11:03:56Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=13764775
dc.identifier.citation Physics and Chemistry of Minerals, 2003, 30, 9, 570-581
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/35520
dc.description.abstract The P21/mC2/m displacive phase transition in the synthetic end-member amphibole Na NaMg Mg5 Si8 O22 (OH)2 has been studied by monitoring changes in unit-cell parameters and the intensities of superlattice reflections at 25–400 C. This amphibole allows investigation of the effects of compositional variations at the A- and B-group sites upon the transition. Polynomial fitting of a 24 Landau potential to the evolution of the order parameter with T yielded a T c of 257 3 C, and Landau coefficients compatible with a second-order transition. Structure refinement of single-crystal data collected at 25, 140, 270 and 370 C allowed modelling of the structural changes as a function of T and symmetry. Crystal-chemical analysis suggests that differences in T c in cummingtonites and in the crystal of this work depend mainly upon the relations between the aggregate ionic radii of the B- and C-group cations.
dc.subject Amphibole
dc.subject HT-XRD
dc.subject Displacive phase transition
dc.subject Synthesis
dc.title THE P21/M ↔ C2/M PHASE TRANSITION IN SYNTHETIC AMPHIBOLE NA NAMG MG5 SI8 O22 (OH)2: THERMODYNAMIC AND CRYSTAL-CHEMICAL EVALUATION
dc.type Статья


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