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Togari, K., Akasaka, M. (1987) Okhotskite, a new mineral, an Mn3+-dominant member of the pumpellyite group, from the Kokuriki mine, Hokkaido, Japan. Mineralogical Magazine, 51 (362) 611-614 doi:10.1180/minmag.1987.051.362.17

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Reference TypeJournal (article/letter/editorial)
TitleOkhotskite, a new mineral, an Mn3+-dominant member of the pumpellyite group, from the Kokuriki mine, Hokkaido, Japan
JournalMineralogical MagazineISSN0026-461X
AuthorsTogari, K.Author
Akasaka, M.Author
Year1987 (October)Volume51
Issue362
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_51/51-362-611.pdf+
DOIdoi:10.1180/minmag.1987.051.362.17Search in ResearchGate
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Mindat Ref. ID1431Long-form Identifiermindat:1:5:1431:5
GUID0
Full ReferenceTogari, K., Akasaka, M. (1987) Okhotskite, a new mineral, an Mn3+-dominant member of the pumpellyite group, from the Kokuriki mine, Hokkaido, Japan. Mineralogical Magazine, 51 (362) 611-614 doi:10.1180/minmag.1987.051.362.17
Plain TextTogari, K., Akasaka, M. (1987) Okhotskite, a new mineral, an Mn3+-dominant member of the pumpellyite group, from the Kokuriki mine, Hokkaido, Japan. Mineralogical Magazine, 51 (362) 611-614 doi:10.1180/minmag.1987.051.362.17
In(1987, October) Mineralogical Magazine Vol. 51 (362) Mineralogical Society
Abstract/NotesAbstractOkhotskite, an Mn3+-dominant pumpellyite-group mineral, is monoclinic, A2/m, a = 8.887, b = 6.000, c = 19.55 Å, β = 97.08°, Z = 1. The formula is(Ca7.63Na0.17K0.01)Σ7.81(Mn2.752+Mg1.10)Σ3.85(Mn4.503+Al1.87Fe1.613+Ti0.02)Σ8.00Si12.13O39.71(OH)16.29,which simplifies to Ca8(Mn2+,Mg)4(Mn3+,Al,Fe3+)8Si12O5∂-n(OH)n. Strong lines in the X-ray powder diffraction pattern are: 4.76(60)(004, 111), 3.87(70)(202), 2.96(100)(115, 300), 2.88(25)(022), 2.72(70)(302), 2.67(45)(3̄04, 3̄11), 2.55(45)(024, 3̄13) and 2.38(45)(304).Its colour is deep orange with a pale orange streak and vitreous lustre. Transparent. Non-fluorescent. H6 (Mohs). Density (calc.) = 3.40 g/cm3. Optically biaxial negative, 2V(meas) = 46(5)°, 2V(calc) = 46°, dispersion indiscernible. Refractive indices: α = 1.782(5), β = 1.820(5), γ = 1.827(5). Orientation: Y = b, c∧Z = 9–14° in acute angle of β. Pleochroism is distinct: X yellow, Y and Z deep orange. Absorption: X < Y < Z.This mineral occurs as fine prisms up to 0.2 mm long and forms aggregates in network veinlets cutting hematite ore from the Kokuriki mine in the Tokoro district, eastern Hokkaido, Japan. Associated minerals are: hematite, piemontite, quartz, neotocite, bementite, apatite, Mn-oxides, inesite and rhodochrosite. The mineral is named okhotskite for the Sea of Okhotsk, along which the mine is located.


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