Miyahisaite, (Sr,Ca)2Ba3(PO4)3F, a new mineral of the hedyphane group in the apatite supergroup from the Shimoharai mine, Oita Prefecture, Japan
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- NISHIO-HAMANE Daisuke
- The Institute for Solid State Physics, the University of Tokyo
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- OGOSHI Yukikazu
- Departments of Earth Science, Faculty of Science, Ehime University
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- MINAKAWA Tetsuo
- Departments of Earth Science, Faculty of Science, Ehime University
書誌事項
- タイトル別名
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- Miyahisaite, (Sr,Ca)<sub>2</sub>Ba<sub>3</sub>(PO<sub>4</sub>)<sub>3</sub>F, a new mineral of the hedyphane group in the apatite supergroup from the Shimoharai mine, Oita Prefecture, Japan
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抄録
Miyahisaite, (Sr,Ca)2Ba3(PO4)3F, a new mineral of the hedyphane group in the apatite supergroup, is found in the Shimoharai mine, Oita Prefecture, Japan. Miyahisaite is colorless and occurs as a pseudomorphic aggregate (up to about 100 μm in size) along with fluorapatite in the quartz matrix in a namansilite-rich layer of the chert. Its hardness is 5 on the Mohs scale, and its calculated density is 4.511 g/cm3. The empirical formula of miyahisaite is (Sr1.366Ca0.717)Σ2.083Ba2.911P3.002O12(F0.898OH0.088Cl0.014)Σ1.00, which is representatively shown as (Sr,Ca)2Ba3(PO4)3F. Its simplified ideal formula is written as Sr2Ba3(PO4)3F, which requires 23.25 wt% SrO, 51.62 wt% BaO, 23.89 wt% P2O5, 2.13 wt% F, and -0.90 wt% F = O, for a total of 100.00 wt%. The mineral is hexagonal with a space group P63/m, unit cell parameters a = 9.921 (2) Å, c = 7.469 (3) Å, and V = 636.7 (3) Å3, and Z = 2. The eight strongest lines in the powder XRD pattern [d (Å), (I/I0), hkl] are 3.427 (16) 102, 3.248 (22) 120, 2.981 (100) 121, 2.865 (21) 300, 1.976 (23) 123, 1.874 (16) 140, 1.870 (15) 004, and 1.864 (17) 402. The mineral was formed by the reaction between fluorapatite and the Ba-bearing fluid that produced the aegirine-rich layer with hydrous Ba-rich minerals during the late-stage activity.
収録刊行物
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- Journal of Mineralogical and Petrological Sciences
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Journal of Mineralogical and Petrological Sciences 107 (3), 121-126, 2012
一般社団法人 日本鉱物科学会
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詳細情報 詳細情報について
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- CRID
- 1390001206546009216
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- NII論文ID
- 10030499194
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- NII書誌ID
- AA11460926
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- BIBCODE
- 2012JMPeS.107..121N
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- COI
- 1:CAS:528:DC%2BC38Xht1GitrvN
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- ISSN
- 13493825
- 13456296
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- 本文言語コード
- en
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- データソース種別
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- JaLC
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