Whelanite, Cu2Ca6[Si6O17(OH)](CO3)(OH)(3)(H2O)(2), an (old) new mineral from the Bawana mine, Milford, Utah

作者：Kampf Anthony R^*; Mills Stuart J; Merlino Stefano; Pasero Marco; McDonald Andrew M; Wray William B; Hindman James R

来源：American Mineralogist, 2012, 97(11-12): 2007-2015.

DOI：10.2138/am.2012.4181

• Whelanite
• new mineral
• crystal structure
• order-disorder structure
• Raman spectroscopy
• Bawana mine
• Milford
• Utah

The new mineral whelanite, Cu2Ca6[Si6O17(OH)](CO3)(OH)(3)(H2O)(2), was approved by the Commission on New Minerals and Mineral Names (1MA) in 1977, but until now a description has not been published. The mineral is orthorhombic with space group Pn2n and cell parameters a = 5.6551(4), b = 3.683(3), c = 27.1372(7) angstrom, V= 565.3(5) angstrom(3), and Z = 1. The mineral occurs with thaumasite, stringhamite, and kinoite in a copper-rich, diopside garnet magnetite skarn at the Bawana mine, Beaver County, Utah, and has also been confirmed to occur at other localities. At the Bawana mine, it is found as irregular clusters and radial aggregates of platy to lath-like crystals up to 1 mm in length, flattened on {001} and elongated on [100]. The color and streak are pale blue and the luster is vitreous. The laths are flexible, but not elastic. Cleavage is perfect on {001} and good on {010}, producing splintery fracture. The Mohs hardness is about 2 1/2. The measured density is 2.74(3) g/cm(3) and the calculated density is 2.737 g/cm(3) based upon the empirical formula. The mineral is biaxial (-), alpha = 1.612(2), beta = I.622(calc), and gamma = 1.626(2), and 2V(meas) = 64(1)degrees. The pleochroism is weak: X= Y(pale blue) %26lt;Z (light blue). The optical orientation is X = a, Y = c, Z = b. A combination of electron microprobe analyses and thennogravimetric analyses (for CO2 and H2O) yielded: CaO 34.46, CuO 12.09, FeO 1.52, SiO2 37.96, CO2 5.93, H2O 8.86, total 100.82 wt%, providing the empirical formula (based on O = 26): CU1.41Fe0.20Ca5.68Si5.84C1.25O26H9.09. Raman spectroscopy shows evidence of (CO3)(2-), (OH)(-), and H2O. The strongest powder X-ray diffraction lines are [d(hkl)I]: 6.79(004)52, 3.072(111)43, 3.013(112)100, 2.921(113)39, 2.802(114)45, 2.522(116,205)44, and 1.839(020,1.1.12)37. The crystal structure (R-1 = 3.89% for 567 F-o %26gt; 4 sigma F) contains two different types of polyhedral layers parallel to {001}, which alternate along [001] and are linked to one another by sharing corners with wollastonite-like silicate chains running parallel [010]. One polyhedral layer, consisting of edge-sharing CaO7 polyhedra, is identical to that in the structures of the tobermorites (tobermorite 9 angstrom, tobermorite 11 angstrom, tobermorite 14A, and clinotobermorite). The other layer is brucite-like, with alternating ribbons of edge-sharing Cu2+O6 and CaO6 octahedra. Disordered CO3 and H2O groups are also located in the interlayer region. The crystal structure of whelanite exhibits OD character.

• 出版日期2012-12