Hostname: page-component-78c5997874-lj6df Total loading time: 0 Render date: 2024-11-13T00:54:05.544Z Has data issue: false hasContentIssue false

Okhotskite, a new mineral, an Mn3+-dominant member of the pumpellyite group, from the Kokuriki mine, Hokkaido, Japan

Published online by Cambridge University Press:  05 July 2018

K. Togari
Affiliation:
Department of Geology and Mineralogy, Faculty of Science, Hokkaido University, Sapporo 060, Japan
M. Akasaka
Affiliation:
Department of Geology and Mineralogy, Faculty of Science, Hokkaido University, Sapporo 060, Japan

Abstract

Okhotskite, 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.

Type
Mineralogy
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1987

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Albee, A.L. and Ray, L. (1970) Anal. Chem. 42, 1408-14.CrossRefGoogle Scholar
Bamba, T. (1984) J. Fac. Sci., Hokkaido Univ. ser. 4, 21, 21-75.Google Scholar
Bancroft, G.M., Maddock, A.G. and Burns, R.G. (1967) Geochim. Cosmochim. Act. 31, 2219-46.CrossRefGoogle Scholar
Bence, A.E. and Albee, A.L. (1968) J. Geol. 76, 382-403.CrossRefGoogle Scholar
Dollase, W.A. (1973) Z. Kristallogr. 138, 41-83.CrossRefGoogle Scholar
Ivanov, O.K., Arkhangel'skaya, V.A., Miroshnikova, L.O. and Shilova, T.A. (1981) Zap. Vses. Mineral. Obsh. 110, 508-12.[in Russian].Google Scholar
Iwata, K. and Tajika, J. (1986) J. Fac. Sci., Hokkaido Univ. ser. 4, 21, 619-44.Google Scholar
Iwata, K., Watanabe, M., Nakamura, K. and Uozurni, S. (1983) Earth Science (Chikyu Kagaku. 37, 225-8.[in Japanese].Google Scholar
Kato, A., Matsubara, S. and Yamamoto, R. (1981) Bull. Mineral. 104, 396-99.Google Scholar
Kiminami, K., Suizu, M. and Kontani, Y. (1983) Earth Science (Chikyu Kagaku. 37, 48-52.[in Japanese].Google Scholar
Mandarino, J.A. (1981) Can. Mineral. 19, 531-4.Google Scholar
Moore, P.B. (1971) Litho. 4, 93-9.CrossRefGoogle Scholar
Palache, C. and Vassar, H.E. (1925) Am. Mineral. 10, 412-18.Google Scholar
Passaglia, E. and Gottardi, G. (1973) Can. Mineral. 12, 219-23.Google Scholar
Research Group of Tokoro Belt (1984) Earth Science (Chikyu Kagaku. 38, 408-19.[in Japanese with English abstract].Google Scholar
Sakakibara, M. (1986) J. Met. Geol. 4, 401-8.CrossRefGoogle Scholar
Shinno, I. and Maeda, Y. (1981) The Report on Earth Sci., College of General Education Kyushu Univ. 22, 13-26.Google Scholar
Togari, K., Akasaka, M. and Kawaguchi, Y. (1986) J. Fac. Sci., Hokkaido Univ. ser. 4, 21, 669-77.Google Scholar