2024 Annual Meeting of Japan Association of Mineralogical Sciences (JAMS)

Presentation information

Poster presentation

R1: Characterization and description of minerals (Joint Session with The Gemmological Society of Japan)

Thu. Sep 12, 2024 12:30 PM - 2:00 PM Entrance Hall (Higashiyama Campus)

12:30 PM - 2:00 PM

[R1-P-10] Mineralogical properties of lautenthalite and wroewolfeite from the Nii mine, Hyogo Prefecture, Japan

*Masayuki Ohnishi, Norimasa Shimobayashi1, Daisuke Nishio-Hamane2, Keiji Shinoda3, Takeshi Hisano (1. Sci., Kyoto Univ., 2. ISSP, Univ. of Tokyo, 3. Sci., Osaka Metro. Univ.)

Keywords:Lautenthalite, Wroewolfeite, Sulfate, Nii mine

Lautenthalite and wroewolfeite have been found in the dump of the Nii mine, Hyogo Prefecture, Japan. The minerals occur in cracks of quartz containing ore minerals such as chalcopyrite, galena and sphalerite.
Lautenthalite is aggregates of platy crystals up to 0.5 mm in length and 0.1 mm in thick. Lautenthalite is always in overgrowth on wroewolfeite. The mineral is blue-green in color with a vitreous luster. It is monoclinic with unit cell parameters of a = 21.557(6), b = 6.019(1), c = 22.467(5) Å, and β = 108.06(3)°. A WDS analysis yields the empirical formula (based on total cations = 7; water by stoichiometry), (Pb0.97Ca0.06)Σ1.03(Cu3.97Zn0.11Mn0.02)Σ4.10(SO4)1.87(OH)6.52·3H2O.
Wroewolfeite is aggregates of platy crystals up to 1 mm in length and 0.1 mm in thick in association with langite, brochantite, linarite and cerussite. The mineral is blue in color with a vitreous luster. It is monoclinic with unit cell parameters of a = 6.042(8), b = 5.637(6), c = 14.45(2) Å, and β = 93.5(1)°. A WDS analysis yields the empirical formula (based on total cations = 5; water by stoichiometry), (Cu3.94Zn0.04Ca0.02Fe0.01Pb0.01Mn0.01)Σ4.04(SO4)0.96(OH)6.14·2H2O. Optically, the mineral is biaxial (-) with refractive indices α = 1.641(2), β = 1.691(2) and γ = 1.701(2), and 2V (calc.) = 47.0°.
R1-P-10