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Benna, P., Tribaudino, M., Bruno, E. (2000) I1̄ – I2/c ferroelastic phase transition in the Ca0.2Pb0.8Al2Si2O8 feldspar as a function of temperature. Mineralogical Magazine, 64 (2) 285-290 doi:10.1180/002646100549184

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Reference TypeJournal (article/letter/editorial)
TitleI1̄ – I2/c ferroelastic phase transition in the Ca0.2Pb0.8Al2Si2O8 feldspar as a function of temperature
JournalMineralogical Magazine
AuthorsBenna, P.Author
Tribaudino, M.Author
Bruno, E.Author
Year2000 (April)Volume64
Issue2
PublisherMineralogical Society
DOIdoi:10.1180/002646100549184Search in ResearchGate
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Mindat Ref. ID243150Long-form Identifiermindat:1:5:243150:9
GUID0
Full ReferenceBenna, P., Tribaudino, M., Bruno, E. (2000) I1̄ – I2/c ferroelastic phase transition in the Ca0.2Pb0.8Al2Si2O8 feldspar as a function of temperature. Mineralogical Magazine, 64 (2) 285-290 doi:10.1180/002646100549184
Plain TextBenna, P., Tribaudino, M., Bruno, E. (2000) I1̄ – I2/c ferroelastic phase transition in the Ca0.2Pb0.8Al2Si2O8 feldspar as a function of temperature. Mineralogical Magazine, 64 (2) 285-290 doi:10.1180/002646100549184
Abstract/NotesAbstractFeldspar of composition Ca0.2Pb0.8Al2Si2O8 (PbF80An20) was synthesized from melt and subsequently isothermally annealed at T = 960°C for 4 days. In situ HT X-ray powder spectra of PbF80An20 feldspar, triclinic I1̄ at room temperature, were collected in the temperature range 20–800°C, and a displacive continuous ferroelastic transition to a I2/c monoclinic phase was observed. An analysis of the symmetry-required components of the spontaneous strain tensor reveals the second order character (β = 0.46 ± 0.02) of the transition with TC = 680 ± 15°C. A linear coupling was observed between the e4 and e6 components of the spontaneous strain. The transition is analogous to those observed, with increasing temperature, along the join An–SrF and in disordered Na-rich alkali feldspars. A comparison with Ca0.2Sr0.8Al2Si2O8 feldspar (TC = 680°C, McGuinn and Redfern, 1997) shows that PbF80An20 has a higher spontaneous strain (εs = 0.028 in PbF80An20vs 0.020 in Ca0.2Sr0.8Al2Si2O8) and a higher e4 component, possibly related to the higher distortion of the non-tetrahedral polyhedron in lead feldspar.


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