 | | Report (issue) | | Hingganite-(Ce) (Ce, Y)BeSiO4(OH) Crystal Data: Monoclinic. Point Group: 2/m. Physical Properties:...detected. As rims on prismatic crystals of hingannite-(Y). D(meas.) = n.d. D(calc.) = [4.82] Optical Properties:...Cell Data: Space Group: P21/a [by analogy to hingganite-(Y)]. c = 4.7505(6) β = 90.416(8)° Z=2 a = 9.8973(1)...= 7.6282(8) X-ray Powder Pattern: Iwaguro Sekizai quarry, Japan. 2.85 (100), 3.13 (86), 2.56 (46), 6...23.27 63.56 9.69 3.49 100.00 (1) Iwaguro Sekizai quarry, Japan; by electron microprobe, BeO calculated |  | | Report (issue) | | Hingganite-(Y) (Y, Yb, Er)BeSiO4(OH) Crystal Data: Monoclinic. Point Group: 2/m. Stout prismatic crystals...Vitreous. Optical Class. Biaxial (+). Orientation: Y = b; Z ^ c = 6°-13°; Z ^ a = 14°. Dispersion: r <...(1) Greater Khingan Range, China; corresponds to (Y 0.33Ce0.21La0.16Nd0.10RE0.13)∑=0.93 [(K:Na)0.07Fe3+0...massif (Kola Peninsula, Russia). Association: Hingganite-(Ce), quartz, potassium feldspar, albite, zinnwaldite...stokesite, fluorite, chlorite, titanite (Tahara area, Japan); aegirine, zircon, quartz (Mt. Malosa, Malawi) |  | MIYAWAKI, Ritsuro, NAKAI, Izumi, NAGASHIMA, Kozo, OKAMOTO, Akiyoshi, ISOBE, Toshio (1987) The first occurences of hingganite, hellandite and wodginite in Japan. Journal of the Mineralogical Society of Japan, 18 (1) 17-30 doi:10.2465/gkk1952.18.17 | Journal (article/letter/editorial) | | occurences Ritsuro ラ ン ド石,ウ 泉,長 島弘 三 of hingganite, MIYAWAKI, Akiyoshi ォ ッジナ石 ・岡 本 鑑 吉 hellandite...in Japan. NAGASHIMA, Toshio ISOBE type pegmatite Abstract Hingganite, hellandite Hirukawa-mura...Hirukawa-mura, and Ena-gun, wodginite Gifu 1.13, were found as associated and an colorless unknown ...c=4.792(4) •ð, ƒÀ=90.06(4)•‹; at Tahara, (Y1.22Ca0.26•c) (hingganite-(Ce)) group flourite. given a...24 occurs Hingganite-(Ce), Hell Wodginite, quarries hingganite, stokesite, hingganite. occurs |  | | Journal (article/letter/editorial) | | 2 1 0 } , { 0 1 0 } , a n d l e s sc o m m o n l y{ 1 0 0 } , { 1 3 0 } , {120}, {230]t {540}, and {320}...zvz: 63'(calc.);pleochroismX : dark greenish-blue, Y : grcen, 7 : pale yellowishbrown. X-ray single-crystal...constitutesthe secondoccurrenceof wiiLlfingite. As well, "y-Zn(OH), is present as a white radiating acicular mineral...containing the Zn(OH), polymorphs is in a limestone quarry at Milltown, near Ashover, Derbyshire, L.D. Arkhipova...chlorite. Hingganite-(Y) from a nearby quarry also is described. Discussion.Related to hingganite-(Y) [xinganite |  | | Book (edition) | | Strunz since 1941 (Strunz and Nickel 2001): • Subsidim-y anions (OH,F,O) are positioned before the complex...(province), co. (county), munic. (municipio), pref. (prefecture), dept. (departement), dept. (departamento),...Mineralogical Abstracts MJJ - Mineralogical Journal of Japan MM - Mineralogical Magazine MP - Mineralogy and...ardennite, Triclinic. ah,c = 8. 4+, 11.12. 7.28, o.,~,y = 90°53', hollandite. and shattuckite, etc., in brownish...Menzenschwand Scbwarzwald Mts., in the Sailauf quarry, Spessart Mts., Bavaria. both Germany, and from |  | Gaines, Richard V., Skinner, H. Catherine W., Foord, Eugene E., Mason, Brian, Rosenzweig, Abraham, King, Vandall T. (1997) Dana's New Mineralogy (8th ed.) Wiley-Interscience. p.1872 | Book (edition) | | California. Akira Kato: National Science Museum, Tokyo, Japan. Petr Korbel: Dept. of Mineralogy, National Museum...example, tritomite-(Ce) and tritomite-(Y) are end members [Ce+Y] in the tritomite series [AM 51:152(1966)]...nal order detectable by diffract at least a implies y generall here use fied exhibits external faces, but...where h, k and] are positive or negative, unequal y elesymmetr all by upon acted are faces al the general...spacing, and subscripted by the relative intensit y from 10 down to 1. The pattern is preceded by the |
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