Secondary phosphates in montebrasite and amblygonite from Nagatare, Fukuoka Prefecture, Japan

Yohei Shirose, Seiichiro Uehara

研究成果: ジャーナルへの寄稿レター

2 引用 (Scopus)

抄録

Montebrasite and amblygonite in an Li-Cs-Ta enriched (LCT) pegmatite from Nagatare, Fukuoka Prefecture, Japan, contain various alteration minerals: fluorapatite, crandallite, goyazite, waylandite, wardite, viitaniemiite, morinite, muscovite, lepidolite, and cookeite. They are associated with lacroixite, quartz, and topaz. Among these minerals, wardite, viitaniemiite, morinite, and lacroixite are newly discovered in Japan. The secondary phosphates and fine-grained mica form fine veins along cleavages and composition planes of polysynthetic twins in the montebrasite and amblygonite. Lacroixite has a different texture from other phosphates, which suggests a possibility of exsolution within montebrasite-amblygonite series. Various secondary phosphates show Ca-, Na- and Sr-metasomatism with leaching of Li, and the formation of low-F montebrasite from montebrasite-amblygonite series indicates an F-OH exchange. However, fluorapatite, morinite, and viitaniemiite crystallized in an F-rich environment. Montebrasite-amblygonite series minerals undergo an acidic alteration to muscovite in the last stage, which is the same process that other Li minerals undergo, such as tourmaline and spodumene.

元の言語英語
ページ(範囲)103-108
ページ数6
ジャーナルJournal of Mineralogical and Petrological Sciences
109
発行部数2
DOI
出版物ステータス出版済み - 1 1 2014

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Japan
fluorapatite
phosphates
minerals
phosphate
muscovite
mineral
goyazite
crandallite
topaz
mineral alteration
spodumene
tourmaline
exsolution
pegmatite
metasomatism
mica
cleavage
leaching
texture

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geology

これを引用

Secondary phosphates in montebrasite and amblygonite from Nagatare, Fukuoka Prefecture, Japan. / Shirose, Yohei; Uehara, Seiichiro.

:: Journal of Mineralogical and Petrological Sciences, 巻 109, 番号 2, 01.01.2014, p. 103-108.

研究成果: ジャーナルへの寄稿レター

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abstract = "Montebrasite and amblygonite in an Li-Cs-Ta enriched (LCT) pegmatite from Nagatare, Fukuoka Prefecture, Japan, contain various alteration minerals: fluorapatite, crandallite, goyazite, waylandite, wardite, viitaniemiite, morinite, muscovite, lepidolite, and cookeite. They are associated with lacroixite, quartz, and topaz. Among these minerals, wardite, viitaniemiite, morinite, and lacroixite are newly discovered in Japan. The secondary phosphates and fine-grained mica form fine veins along cleavages and composition planes of polysynthetic twins in the montebrasite and amblygonite. Lacroixite has a different texture from other phosphates, which suggests a possibility of exsolution within montebrasite-amblygonite series. Various secondary phosphates show Ca-, Na- and Sr-metasomatism with leaching of Li, and the formation of low-F montebrasite from montebrasite-amblygonite series indicates an F-OH exchange. However, fluorapatite, morinite, and viitaniemiite crystallized in an F-rich environment. Montebrasite-amblygonite series minerals undergo an acidic alteration to muscovite in the last stage, which is the same process that other Li minerals undergo, such as tourmaline and spodumene.",
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AB - Montebrasite and amblygonite in an Li-Cs-Ta enriched (LCT) pegmatite from Nagatare, Fukuoka Prefecture, Japan, contain various alteration minerals: fluorapatite, crandallite, goyazite, waylandite, wardite, viitaniemiite, morinite, muscovite, lepidolite, and cookeite. They are associated with lacroixite, quartz, and topaz. Among these minerals, wardite, viitaniemiite, morinite, and lacroixite are newly discovered in Japan. The secondary phosphates and fine-grained mica form fine veins along cleavages and composition planes of polysynthetic twins in the montebrasite and amblygonite. Lacroixite has a different texture from other phosphates, which suggests a possibility of exsolution within montebrasite-amblygonite series. Various secondary phosphates show Ca-, Na- and Sr-metasomatism with leaching of Li, and the formation of low-F montebrasite from montebrasite-amblygonite series indicates an F-OH exchange. However, fluorapatite, morinite, and viitaniemiite crystallized in an F-rich environment. Montebrasite-amblygonite series minerals undergo an acidic alteration to muscovite in the last stage, which is the same process that other Li minerals undergo, such as tourmaline and spodumene.

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