Putnisite, SrCa4(CO3)8SO4(OH)16·25H2O, a new mineral from Western Australia: description and crystal structure: Description and crystal structure

P Elliott, G Giester, R Rowe, Allan Pring

    Research output: Contribution to journalArticle

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    Abstract

    Putnisite, SrCa4Cr3+ 8 (CO3)8SO4(OH)16.25H 2O, is a new mineral from the Polar Bear peninsula, Southern Lake Cowan, Western Australia, Australia. The mineral forms isolated pseudocubic crystals up to 0.5 mm in size in a matrix composed of quartz and a near amorphous Cr silicate. Putnisite is translucent, with a pink streak and vitreous lustre. It is brittle and shows one excellent and two good cleavages parallel to {100}, {010} and {001}. The fracture is uneven and the Mohs hardness 12. The measured density is 2.20(3) g/cm3 and the calculated density based on the empirical formula is 2.23 g/cm3. Optically, putnisite is biaxial negative, with a = 1.552(3), b = 1.583(3) and g = 1.599(3) (measured in white light). The optical orientation is uncertain and pleochroism is distinct: X pale bluish grey, Y pale purple, Z pale purple. Putnisite is orthorhombic, space group Pnma, with a = 15.351(3), b = 20.421(4) Å , c = 18.270(4) Å , V = 5727(2) Å 3 (single-crystal data), and Z = 4. The strongest five lines in the X-ray powder diffraction pattern are [d(Å)(I)(hkl)]: 13.577 (100) (011), 7.659 (80) (200), 6.667 (43) (211), 5.084 (19) (222, 230), 3.689 (16) (411). Electron microprobe analysis (EMPA) gave (wt.%): Na2O 0.17, MgO 0.08, CaO 10.81, SrO 5.72, BaO 0.12, CuO 0.29, Cr2O3 31.13, SO3 3.95, SiO2 0.08, Cl 0.28, CO2calc 17.94, H2Ocalc 30.30, O=Cl 0.06, total 100.81. The empirical formula, based on O + Cl = 69, is: Cr3+ 8.02Ca3.78Sr1.08Na0.11Cu2+ 0.07Mg0.04Ba0.02[(SO4)0.96(SiO 4)0.03]0.99 (CO3)7.98(OH)16.19Cl0.15.24.84H2O. The crystal structure was determined from single-crystal X-ray diffraction data (MoKa, CCD area detector and refined to R1 = 5.84% for 3181 reflections with F0 > 4sF. Cr(OH)4O2 octahedra link by edge-sharing to form an eight-membered ring. A 10-coordinated Sr2+ cation lies at the centre of each ring. The rings are decorated by CO3 triangles, each of which links by corner-sharing to two Cr(OH)4O2 octahedra. Rings are linked by Ca(H2O)4O4 polyhedra to form a sheet parallel to (100). Adjacent sheets are joined along [100] by corner-sharing SO4 tetrahedra. H2O molecules occupy channels that run along [100] and interstices between slabs. Moderate to weak hydrogen bonding provides additional linkage between slabs.

    Original languageEnglish
    Pages (from-to)131-144
    Number of pages14
    JournalMineralogical Magazine
    Volume78
    Issue number1
    DOIs
    Publication statusPublished - 2014

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