New Minerals from the Redmond Mine, North Carolina, USA: IV. Haywoodite and Hanahanite, Two New Minerals Containing Gordaite-Like Sheets
Author:
Kampf Anthony R.1, Smith Jason B.2, Hughes John M.3, Ma Chi4, Emproto Christopher5
Affiliation:
1. Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA 2. 2148 McClintock Road, Charlotte, North Carolina 28205, USA 3. Department of Geology, University of Vermont, 180 Colchester Ave., Burlington, Vermont 05405, USA 4. Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, California 91125, USA 5. Department of Earth and Environmental Sciences, University of Michigan, 1100 North University Avenue, Ann Arbor, Michigan 48109, USA
Abstract
Abstract
The new minerals haywoodite, [Pb(H2O)10)][Zn12(OH)20(H2O)(SO4)3] (IMA2021-115), and hanahanite, [Zn8(OH)14(SO4)]·3H2O (IMA2022-012), were found in the Redmond mine, Haywood County, North Carolina, USA, where they occur in a highly unusual secondary assemblage that comprises a variety of rare Pb-Zn-Cu sulfates, thiosulfates, and carbonates. Haywoodite has the following properties: colorless to pale pink pseudohexagonal tablets and barrel-like prisms up to about 0.5 mm in diameter; white streak; vitreous luster; brittle; Mohs hardness 2½; curved and stepped fracture; one perfect cleavage on {011}; 3.27(2) g/cm3 measured density; biaxial (−) with 1.588(2), β = 1.600(2), γ = 1.607(2), and 2V (meas.) = 76(2)°. Hanahanite has the following properties: light blue prisms up to 0.3 mm in length; white streak; vitreous luster; brittle; Mohs hardness 3; curved fracture; one very good cleavage on {001}; 3.28(2) g/cm3 measured density; uniaxial (−) with ω = 1.636(3) and ε = 1.620(3). Electron probe microanalyses provided the empirical formulae Pb1.36Zn11.97S3.00O43H41.33 and (Zn6.69Cu1.27Co0.01)Σ7.97S1.00O21H20.04 for haywoodite and hanahanite, respectively. Haywoodite is triclinic, P1¯, a = 8.35298(19), b = 13.2769(7), c = 18.2744(13) Å, α = 92.427(8), β = 90.419(6), γ = 108.214(4)°, V = 1922.94(18) Å3, and Z = 2. Hanahanite is hexagonal, P63, a = 8.312(2), c = 15.295(2) Å, V = 915.2(5) Å3, and Z = 2. The structures of haywoodite (R1 = 0.037 for 6876 I > 2σI) and hanahanite (R1 = 0.065 for 772 I > 2σI) both contain gordaite-like sheets. In the haywoodite structure, a disordered interlayer region contains approximately one Pb and ten H2O pfu. In the hanahanite structure, ZnO4 tetrahedra in adjacent sheets are linked by sharing corners and the interlayer region only contains an H2O group.
Publisher
Mineralogical Association of Canada
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