7T wollastonite from Fuka, Okayama Prefecture

A 7T wollastonite was found at Fuka, Okayama Prefecture. Based on film intensity data, its stacking sequence has been found as (TTGTGTG). Here, T represents a (100) slab of wollastonite which is in continuous position with respect to the preceding one, and G a slab displaced by b⁄2. The structure ma...

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Published inMineralogical Journal Vol. 9; no. 3; pp. 169 - 181
Main Authors HENMI, Chiyoko, KUSACHI, Isao, KAWAHARA, Akira, HENMI, Kitinosuke
Format Journal Article
LanguageEnglish
Published Japan Association of Mineralogical Sciences 1978
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Abstract A 7T wollastonite was found at Fuka, Okayama Prefecture. Based on film intensity data, its stacking sequence has been found as (TTGTGTG). Here, T represents a (100) slab of wollastonite which is in continuous position with respect to the preceding one, and G a slab displaced by b⁄2. The structure may be regarded as a mixed-layer structure composed of three 2M and one 1T. The structure gave R=0.13 for 65 hk0 reflexions observed. The lattice constants are a=54.3±0.3 Å, b=7.30±0.03 Å, c=7.08±0.03 Å, α=90.0±0.2°, β=95.5±0.2°, and γ=92.1±0.2°.
AbstractList A 7T wollastonite was found at Fuka, Okayama Prefecture. Based on film intensity data, its stacking sequence has been found as (TTGTGTG). Here, T represents a (100) slab of wollastonite which is in continuous position with respect to the preceding one, and G a slab displaced by b⁄2. The structure may be regarded as a mixed-layer structure composed of three 2M and one 1T. The structure gave R=0.13 for 65 hk0 reflexions observed. The lattice constants are a=54.3±0.3 Å, b=7.30±0.03 Å, c=7.08±0.03 Å, α=90.0±0.2°, β=95.5±0.2°, and γ=92.1±0.2°.
Author HENMI, Chiyoko
KUSACHI, Isao
HENMI, Kitinosuke
KAWAHARA, Akira
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Cites_doi 10.1107/S0365110X53002428
10.2183/pjab1945.45.913
10.1073/pnas.47.12.1884
10.1038/physci245043a0
10.1524/zkri.1968.127.1-4.291
10.1007/BF00387956
10.2465/minerj.8.374
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Title 7T wollastonite from Fuka, Okayama Prefecture
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