Distribution of chromium among the octahedral sites in chromian epidote from Iratsu, central Shikoku, Japan

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概要

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• The crystal structures of chromian epidotes from the Sambagawa metamorphic rocks, central Shikoku, Japan, were refined using single-crystal data to investigate the distribution of chromium among the three independent octahedral sites. On the basis of the electron probe microanalysis of the chromian epidotes on the polished surface of thin sections, three chromian epidote grains in a thin section were selected for X-ray intensity data collection, and their Cr2O3 values were as much as 1.79, 4.99, and 4.74 wt%, respectively, which led to values of 0.113, 0.315, and 0.299 Cr apfu, respectively. Nevertheless, their Fe2O3 contents were nearly constant (8.1-8.7 wt%, 0.49-0.52 Fe apfu) and their SrO contents were not significant (1.8-3.2 wt%, 0.08-0.15 Sr apfu). The selected chromian epidote grains were picked out using a binocular optical microscope from the thin sections, and were labeled as CrEp1, CrEp2, and CrEp3, respectively. The oxidation state of chromium was found to be trivalent by the optical spectrum. 57Fe Mössbauer doublets with isomer shift of 0.28-0.53 mm/sec and quadrupole splitting of 1.77-2.24 mm/sec indicate an exclusive distribution of Fe3+ at the M3 site. The crystal structure of CrEp1 [a = 8.8815(6), b = 5.5956(5), c = 10.1532(5) Å, β = 115.159(2)], CrEp2 [a = 8.9165(4), b = 5.6226(2), c = 10.1728(5) Å, β = 115.2365(9)], and CrEp3 [a = 8.895(2), b = 5.610(1), c = 10.146(2) Å, β = 115.177(2)] were refined using 1145, 1853 and 1438 unique reflections, respectively, and the calculations converged at R factors of 5.8%, 6.6%, and 3.2%, respectively. The resulting structural formula were: [Ca]A1[Ca0.86Sr0.14]A2[Al]M1[Al]M2[Al0.43Cr3+0.09Fe3+0.48]M3Si3O12(OH) for CrEp1, [Ca]A1[Ca0.90Sr0.10]A2[Al0.86Cr3+0.14]M1[Al]M2[Al0.34Cr3+0.17Fe3+0.49]M3Si3O12(OH) for CrEp2, and [Ca]A1[Ca0.88Sr0.12]A2[Al0.90Cr3+0.10]M1[Al]M2[Al0.37Cr3+0.12Fe3+0.51]M3Si3O12(OH) for CrEp3. The selective distribution of Cr3+ at the M3 site in CrEp1, and the KD values (KD = (Cr3+/Al)M1/(Cr3+/Al)M3) of 0.35(3) for CrEp2 and 0.41(3) for CrEp3 show that the preference of Cr3+ in the octahedral sites is M3 > M1 » M2. The variations in the M1-Oi and M3-Oi distances indicate an equidimensional expansion of the M1O6 and M3O6 octahedra by the substitution of Cr3+(+ Fe3+) for Al3+.

• 日本鉱物科学会の論文
• 2007-08-01

著者

• AKASAKA Masahide

  Department of Geoscience, Faculty of Science and Engineering, Shimane University

• IKEDA Ko

  Department of Advanced Materials Science and Engineering, Yamaguchi University

• KYONO Atsushi

  Division of Earth Evolution Sciences, Graduate School of Life and Environmental Sciences, University

• MAKINO Kuniaki

  Department of Geology, Shinshu University

• Kyono Atsushi

  Division Of Earth Evolution Sciences Graduate School Of Life And Environmental Sciences University O

• Makino Kuniaki

  Dep. Of Geological Sciences Fac. Of Sci. Shinshu Univ.

• Makino Kuniaki

  Department Of Geological Sciences Faculty Of Science Shinshu University

• Akasaka Masahide

  Department Of Materials Creation And Circulation Technology Graduate School Of Science And Engineeri

• Akasaka Masahide

  Department Of Geoscience Faculty Of Science And Engineering Shimane University

• Nagashima Mariko

  Department Of Materials Creation And Circulation Technology Interdisciplinary Graduate School Of Sci

• Nagashima Mariko

  Department Of Materials Creation And Circulation Technology Graduate School Of Science And Engineeri

• Ikeda Ko

  Department Of Advanced Materials Science And Engineering Yamaguchi University

• Nagashima Mariko

  Mineralogical Crystallography Inst. Of Geological Sciences Univ. Of Bern

• Nagashima Mariko

  Department Of Earth Science Graduate School Of Science And Engineering Yamaguchi University

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