Niigataite, CaSrAl3(Si2O7)(SiO4)O(OH): Sr-analogue of clinozoisite, a new member of the epidote group from the Itoigawa-Ohmi district, Niigata Prefecture, central Japan
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Accession number;03A0606062
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| Title;Niigataite, CaSrAl3(Si2O7)(SiO4)O(OH): Sr-analogue of clinozoisite, a new member of the epidote group from the Itoigawa-Ohmi district, Niigata Prefecture, central Japan |
| Author;
MIYAJIMA H
(Fossa Magna Museum, Niigata, Jpn)
MATSUBARA S
(National Sci. Museum, Tokyo, Jpn)
MIYAWAKI R
(National Sci. Museum, Tokyo, Jpn)
HIROKAWA K
(Suihodo Co. Ltd., Niigata, Jpn)
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Journal Title;J Mineral Petrol Sci
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Journal Code:G0150B
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ISSN:1345-6296
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VOL.98;NO.3;PAGE.118-129(2003)
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| Figure&Table&Reference;FIG.6, TBL.8, REF.38 |
| Pub. Country;Japan |
| Language;English |
| Abstract;Niigataite, CaSrAl3(Si2O7)(SiO4)O(OH), is a new member of the epidote group. It is monoclinic, P21/m, a=8.890(4), b=5.5878(18), c=10.211(4).ANGS., b=115.12(3).DEG., V=459.3(3).ANGS.3 and Z=2. The 8 strongest X-ray powder diffractions are dobs(.ANGS.)(I/I0)(hkl): 2.90(100)(113), 2.79(48)(020), 2.70(26)(013), 3.22(25)(201), 2.11(24)(221), 2.60(24)(311), 5.05(23)(102) and 1.397(22)(040). Electron microprobe analysis gave the composition SiO2 35.49, TiO2 0.75, Al2O3 24.86, Fe2O3 7.08, MnO 0.22, MgO 0.07, CaO 14.09, SrO 14.75, H2O (calc.) 1.77 total 99.08wt%, corresponding to a formula Ca1.00(Sr0.72Ca0.28).SIGMA.1.00(Al2.48Fe0.45Ti0.05Mn0.02Mg0.01).SIGMA.3.01Si3.00O13. H calculated on the basis of H=1 and O=13 per unit formula. It is transparent, pale gray with a yellowish green tint. Cleavage is perfect on one direction. Streak is white. The Vickers microhardness is 642-907kg/mm2 (100g load) corresponding to Mohs' 5-5.5. The calculated density is 3.63g/cm3. It occurs as anhedral grains in close association with chlorite and diaspore in druse of prehnite rock in the seashore of Miyabana, Ohmi Town, Niigata Prefecture, central Japan. Niigataite is considered to be crystallized under the presence of Sr-rich metamorphic solution in the late stage of the formation of prehnite rock. Sr enrichment is caused by crystallization of prehnite, which is the most abundant phase having no acceptability of Sr. (author abst.) |
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