Chiyoko Henmi
Okayama University
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Mineralogical Magazine | 1998
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
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
Shinsuke Saburi; Akira Kawahara; Chiyoko Henmi; Isao Kusachi; Kuniaki Kihara
Mineralogical Magazine | 1995
Chiyoko Henmi; Isao Kusachi; Kitinosuke Henmi
Mineralogical Magazine | 1994
Isao Kusachi; Chiyoko Henmi
American Mineralogist | 1983
Chiyoko Henmi; Akira Kawahara; Kitinosuke Henmi; Isao Kusachi; Yoshio Takéuchi
The Journal of the Japanese Association of Mineralogists,Petrologists and Economic Geologists | 1984
Isao Kusachi; Chiyoko Henmi; Kitinosuke Henmi
Mineralogical Journal | 1976
Shinsuke Saburi; Isao Kusachi; Chiyoko Henmi; Akira Kawahara; Kitinosuke Henmi; Isao Kawada
Mineralogical Journal | 1975
Isao Kusachi; Chiyoko Henmi; Akira Kawahara; Kitinosuke Henmi
Mineralogical Journal | 1977
Chiyoko Henmi; Isao Kusachi; Akira Kawahara; Kitinosuke Henmi