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

dc.contributor.authorCámara F.
dc.contributor.authorOberti R.
dc.contributor.authorIezzi G.
dc.contributor.authorDella Ventura G.
dc.date.accessioned2022-02-17T11:03:56Z
dc.date.available2022-02-17T11:03:56Z
dc.date.issued2003
dc.description.abstractThe 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.identifierhttps://elibrary.ru/item.asp?id=13764775
dc.identifier.citationPhysics and Chemistry of Minerals, 2003, 30, 9, 570-581
dc.identifier.issn0342-1791
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/35520
dc.subjectAmphibole
dc.subjectHT-XRD
dc.subjectDisplacive phase transition
dc.subjectSynthesis
dc.titleTHE P21/M ↔ C2/M PHASE TRANSITION IN SYNTHETIC AMPHIBOLE NA NAMG MG5 SI8 O22 (OH)2: THERMODYNAMIC AND CRYSTAL-CHEMICAL EVALUATION
dc.typeСтатья

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