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Featured researches published by Chiyoko Henmi.


Mineralogical Magazine | 1998

Parasibirskite, a new mineral from Fuka, Okayama Prefecture, Japan

Isao Kusachi; Yasushi Takechi; Chiyoko Henmi; Shoichi Kobayashi

Abstract Parasibirskite, with the ideal formula Ca2B2O5 · H2O, is a new mineral species found at Fuka, Okayama Prefecture, Japan. It is a polymorph of sibirskite, CaHBO3, and occurs as subparallel aggregates of tabular crystals up to 40 × 20 × 3 μm in size. Associated minerals are takedaite, olshanskyite, sibirskite, frolovite and calcite. The mineral is white, and has a weak pearly luster. Optically, the mineral is biaxial positive, α 1.556(2), β 1.593(2), γ 1.663(2) (λ 589 nm). The Vickers microhardness of aggregates is 121 kg mm-2. The mineral is monoclinic with space group of P21/m a 6.722(4), b 5.437(2), c 3.555(2) Å, β 93.00(5)°, V 129.8(2) Å3. The strongest lines in the X-ray powder pattern [d in Å (I)(hkl)] are 2.237(100)(300), 6.73(70)(100), 2.975(60)(011), 3.354(30)(200), 2.855(20)(210) and 1.776(20) (002). Wet chemical analysis, electron-microprobe analysis and ICP emission spectrometry give the values CaO 56.06 %, B2O3 34.10 %, H2O 9.97 % and total 100.13%. The empirical formula calculated on the basis of O = 6 is Ca1.985B1.945O4.901 · 1.099H2O, for Z = 1, Dcalc 2.54 and Dmeas 2.50(1) g cm-3. Parasibirskite is formed by hydrothermal alteration of takedaite.


Mineralogical Magazine | 1995

Kusachiite, CuBi2O4, a new mineral from Fuka, Okayama Prefecture, Japan

Chiyoko Henmi

Abstract Kusachiite, CuBi2O4, has been found in a calcite vein cutting gehlenite-spurrite skarns at Fuka, Okayama Prefecture. It is associated with calcite, henmilite, sillenite, bakerite, tenolite, bultfonteinite, apophyllite, cuspidine and thaumasite. Kusachiite occurs as prismatic crystals or globular aggregates of platy crystals. It is black, opaque with a metallic lustre. Kusachiite is tetragonal with space group P4/ncc, a = 8.511(2), c = 5.823(2) Å, Z = 4. The strongest lines in the X-ray powder pattern [d in Å (I)(hkl)] are 3.191 (100)(211), 2.695 (18)(310), 1.947 (18)(411), 4.26 (17)(200), 2.913 (16)(002), 2.404 (13)(202), 1.728 (12)(213), and 1.652 (9)(332). The Mohs hardness is 4.5, and the density is 8.5(3) g/cm3 (meas.) and 8.64 g/cm3 (calc.). Cleavage is perfect on { 110}. Six electron probe analyses gave the following mean values CuO 13.91, Bi2O3 86.00 and total 99.91 in wt.%. The empirical formula calculated on the basis of O = 4 is Cu0.960Bi2.027O4 with the simplified formula CuBi2O4.


Mineralogical Journal | 1977

The refinement of the crystal structure of cuspidine

Shinsuke Saburi; Akira Kawahara; Chiyoko Henmi; Isao Kusachi; Kuniaki Kihara


Mineralogical Magazine | 1995

Morimotoite, Ca 3 TiFe (super 2+) Si 3 O 12 , a new titanian garnet from Fuka, Okayama Prefecture, Japan

Chiyoko Henmi; Isao Kusachi; Kitinosuke Henmi


Mineralogical Magazine | 1994

Nifontovite and olshanskyite from Fuka, Okayama Prefecture, Japan

Isao Kusachi; Chiyoko Henmi


American Mineralogist | 1983

The 3T, 4T and 5T polytypes of wollastonite from Kushiro, Hiroshima Prefecture, Japan

Chiyoko Henmi; Akira Kawahara; Kitinosuke Henmi; Isao Kusachi; Yoshio Takéuchi


The Journal of the Japanese Association of Mineralogists,Petrologists and Economic Geologists | 1984

An oyelite-bearing vein at Fuka, the Town of Bitchu, Okayama Prefecture

Isao Kusachi; Chiyoko Henmi; Kitinosuke Henmi


Mineralogical Journal | 1976

Refinement of the structure of rankinite.

Shinsuke Saburi; Isao Kusachi; Chiyoko Henmi; Akira Kawahara; Kitinosuke Henmi; Isao Kawada


Mineralogical Journal | 1975

The structure of rankinite

Isao Kusachi; Chiyoko Henmi; Akira Kawahara; Kitinosuke Henmi


Mineralogical Journal | 1977

Fukalite, a new calcium carbonate silicate hydrate mineral

Chiyoko Henmi; Isao Kusachi; Akira Kawahara; Kitinosuke Henmi

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Shoichi Kobayashi

Kurashiki University of Science and the Arts

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Yasushi Takechi

American Museum of Natural History

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