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005     20250730144923.0
024 7 _ |a 10.3749/canmin.52.1.91
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024 7 _ |a 1499-1261
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024 7 _ |a 1499-1276
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100 1 _ |a Beirau, T.
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245 _ _ |a Temperature-induced P21/c to C2/c phase transition in partially amorphous (METAMICT) titanite revealed by Raman spectroscopy
260 _ _ |a Ottawa
|c 2014
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500 _ _ |a (c) Mineralogical Association of Canada. Post referee fulltext in progress.
520 _ _ |a In situ temperature-dependent Raman spectroscopic measurements of two partially amorphous (metamict) titanite samples with accumulated radiation doses ~1.2 × 1018 α-events/g (E2335) and ~2.2 ×1018 α-events/g (M28696) and amorphous fractions of 0.24 and 0.5, respectively, provide evidence for a thermally induced transformation analogous to the phase transition P21/c ↔ C2/c, which is characteristic of endmember titanite (CaTiSiO5). Quantitative analysis of the temperature evolution of the wavenumbers and widths of Raman-active vibrations in both partially amorphous titanites reveals an anomaly near 500 K which is consistent with the P21/c ↔ C2/c phase-transition temperature of titanite close to its endmember composition. The observed spectral changes are not due to structural recovery of the radiation-damaged structure because synchrotron X-ray diffraction experiments of M28696 titanite show that relevant recrystallization occurs at annealing temperatures above 600 K. The structural transformation near 500 K is observed by Raman spectroscopy even in heavily radiation-damaged and chemically inhomogeneous titanite (M28696). The microstructure of the samples consists of coexisting crystalline and amorphous domains, with the P21/c to C2/c phase-transition occurring in the latter.
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700 1 _ |a Mihailova, B.
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700 1 _ |a Malcherek, T.
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700 1 _ |a Paulmann, C.
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700 1 _ |a Bismayer, U.
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700 1 _ |a Groat, L. A.
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773 _ _ |a 10.3749/canmin.52.1.91
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