M. Nagashima, T. Imaoka, T. Kano, J. Kimura, Q. Chang, Takashi Matsumoto
{"title":"Ferro-ferri-holmquistite, □Li2(Fe2+3Fe3+2)Si8O22(OH)2, Fe2+Fe3+ analogue of holmquistite, from the Iwagi islet, Ehime, Japan","authors":"M. Nagashima, T. Imaoka, T. Kano, J. Kimura, Q. Chang, Takashi Matsumoto","doi":"10.5194/ejm-34-425-2022","DOIUrl":null,"url":null,"abstract":"Abstract. Ferro-ferri-holmquistite (IMA2022-020), ideal formula\n□Li2(Fe32+Fe23+)Si8O22(OH)2, was\nfound in albitized granite from the Iwagi islet, Ehime, Japan.\nFerro-ferri-holmquistite is a CFe2+Fe3+ analogue of\nholmquistite and belongs to the lithium-subgroup amphiboles. It commonly\noccurs as acicular aggregate and/or isolated crystals in quartz, albite and\nK-feldspar and is blue with a bluish-grey streak and a vitreous luster. It\nhas a Mohs hardness of 5 1/2. Its cleavage is perfect on\n{210}. Measured and calculated densities are\nDmeas.=3.2 g cm−3 and Dcalc.=3.317 g cm−3,\nrespectively. Ferro-ferri-holmquistite is optically biaxial (-), with\nα=1.685, β=1.713 and γ=1.727, and is\npleochroic, with X= pale blue ∼ pale yellowish blue, Y= deep blue ∼ brownish blue and Z= deep blue ∼ deep bluish violet; X>Z>Y. The magnetic\nsusceptibility is similar to the associated biotite.\nFerro-ferri-holmquistite is insoluble in HCl, HNO3 and H2SO4.\nThe empirical formula calculated on the basis of Σ(C+T) = 13 on the results obtained by electron\nmicroprobe analyzer (EPMA), and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) is\nA(K0.01Na0.06)Σ0.07B(Li1.95Na0.04Ca0.01)Σ2.00C(Fe2.822+Fe1.393+Al0.51Mg0.22Mn0.052+Ti0.01)Σ5.00T(Si7.98Al0.02)Σ8.00O22(OH)1.94F0.06. Structure refinement converged\nto R1= 4.22 %. The space group is orthorhombic Pnma, and the\nunit-cell parameters are a= 18.5437(2) Å, b= 17.9222(1) Å, c= 5.3123(1) Å and V= 1765.51(1) Å3. Based on the refined\nsite occupancies, the structural formula can be written as\nANa0.062M4(Li1.952Na0.048)Σ2.000M1(Fe1.7702+Mg0.230)Σ2.000M2(Fe1.4463+Fe0.1022+Al0.452)Σ2.000M3(Fe0.8912+Mg0.109)Σ1.000TSi8O22(OH)2 (Z= 4). Three OH-stretching IR\nbands, centered at 3614, 3631 and 3644 cm−1, are assigned to the local\nconfiguration M1M1M3= FeFeFe, MgFeFe (including FeMgFe and FeFeMg) and\nMgMgFe (including MgFeMg and FeMgMg), respectively, based on the IR studies\nof the orthorhombic Pnma amphiboles.\n","PeriodicalId":11971,"journal":{"name":"European Journal of Mineralogy","volume":" ","pages":""},"PeriodicalIF":1.8000,"publicationDate":"2022-10-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"European Journal of Mineralogy","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/ejm-34-425-2022","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"MINERALOGY","Score":null,"Total":0}
引用次数: 1
Abstract
Abstract. Ferro-ferri-holmquistite (IMA2022-020), ideal formula
□Li2(Fe32+Fe23+)Si8O22(OH)2, was
found in albitized granite from the Iwagi islet, Ehime, Japan.
Ferro-ferri-holmquistite is a CFe2+Fe3+ analogue of
holmquistite and belongs to the lithium-subgroup amphiboles. It commonly
occurs as acicular aggregate and/or isolated crystals in quartz, albite and
K-feldspar and is blue with a bluish-grey streak and a vitreous luster. It
has a Mohs hardness of 5 1/2. Its cleavage is perfect on
{210}. Measured and calculated densities are
Dmeas.=3.2 g cm−3 and Dcalc.=3.317 g cm−3,
respectively. Ferro-ferri-holmquistite is optically biaxial (-), with
α=1.685, β=1.713 and γ=1.727, and is
pleochroic, with X= pale blue ∼ pale yellowish blue, Y= deep blue ∼ brownish blue and Z= deep blue ∼ deep bluish violet; X>Z>Y. The magnetic
susceptibility is similar to the associated biotite.
Ferro-ferri-holmquistite is insoluble in HCl, HNO3 and H2SO4.
The empirical formula calculated on the basis of Σ(C+T) = 13 on the results obtained by electron
microprobe analyzer (EPMA), and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) is
A(K0.01Na0.06)Σ0.07B(Li1.95Na0.04Ca0.01)Σ2.00C(Fe2.822+Fe1.393+Al0.51Mg0.22Mn0.052+Ti0.01)Σ5.00T(Si7.98Al0.02)Σ8.00O22(OH)1.94F0.06. Structure refinement converged
to R1= 4.22 %. The space group is orthorhombic Pnma, and the
unit-cell parameters are a= 18.5437(2) Å, b= 17.9222(1) Å, c= 5.3123(1) Å and V= 1765.51(1) Å3. Based on the refined
site occupancies, the structural formula can be written as
ANa0.062M4(Li1.952Na0.048)Σ2.000M1(Fe1.7702+Mg0.230)Σ2.000M2(Fe1.4463+Fe0.1022+Al0.452)Σ2.000M3(Fe0.8912+Mg0.109)Σ1.000TSi8O22(OH)2 (Z= 4). Three OH-stretching IR
bands, centered at 3614, 3631 and 3644 cm−1, are assigned to the local
configuration M1M1M3= FeFeFe, MgFeFe (including FeMgFe and FeFeMg) and
MgMgFe (including MgFeMg and FeMgMg), respectively, based on the IR studies
of the orthorhombic Pnma amphiboles.
期刊介绍:
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