Journal
PHYSICS AND CHEMISTRY OF MINERALS
Volume 49, Issue 1, Pages -Publisher
SPRINGER
DOI: 10.1007/s00269-021-01172-4
Keywords
Steudelite; New mineral; Cancrinite group; Feldspathoid; Crystal structure; IR spectroscopy; Sacrofano paleovolcano; Latium
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Funding
- Russian Science Foundation [19-17-00050, AAA-A19-119092390076-7]
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The new mineral steudelite has been discovered in the Sacrofano region of Italy. It forms colorless, thick-tabular, isometric and short-prismatic crystals up to 7 mm across. Steudelite is brittle with a Mohs' hardness of 5 and its chemical composition includes Na2O, K2O, CaO, Al2O3, Fe2O3, SiO2, SO2, SO3, F, Cl, H2O, and -O=Cl,F.
The new cancrinite-group mineral steudelite, ideally (Na-3 square)[(K,Na)(17)Ca-7]Ca-4(Al24Si24O96)(SO3)(6)F-6 center dot 4H(2)O, was discovered in syenite ejectum from the Sacrofano paleovolcano, Latium region, Italy. The associated minerals are sanidine, diopside, andradite, biotite, leucite, hauyne, sacrofanite, biachellaite, liottite, and secondary dioctahedral smectite. Steudelite forms colourless, thick-tabular, isometric and short-prismatic crystals up to 7 mm across. Cleavage is distinct on {10 (1) over bar 0}; perfect parting on {0001} is observed. Steudelite is brittle, with uneven fracture. The Mohs' hardness is 5. Measured and calculated density are equal to 2.51 (1) and 2.511 g cm(-3), respectively. The IR spectrum shows the presence of H2O molecules, SO32- and minor SO42- anionic groups. The chemical composition of steudelite is (wt%; electron microprobe, H2O determined by the modified Penfield method; total sulfur apportioned between SO2 and SO3 based on structural data): Na2O 7.40, K2O, 8.42, CaO 3.54, Al2O3 26.46, Fe2O3 0.18, SiO2 30.96, SO2 4.74, SO3 5.18, F 1.66, Cl 0.84, H2O 1.6, -O=Cl,F - 0.89, total 100.09. The empirical formula is H8.22Na11.06K8.28Ca11.18(Al24.04Fe0.103+Si23.86O96)(SO3)(3.43)(SO4)(3.00)F4.04Cl1.10O3.89. The crystal structure of steudelite is based on the afghanite-type aluminosilicate framework containing a column of cancrinite cages and isolated cancrinite and liottite cages whose populations are {Na3.14Ca0.14 square(0.72)[(H2O,OH)(3.72)Cl-0.28]}, {Ca4F4.02Cl0.60}, and {K8.40Na8.13Ca7.10(SO3)(3.24)(SO4)(2.76)}, respectively. The SO32- and SO42- groups occur in the liottite cage, at two sites with the occupancies (S1)[(SO4)(0.69)(SO3)(0.31)] and (S2)[SO3](2). Steudelite is hexagonal, space group P-62c, with a = 12.89529 (15), c = 21.2778 (3) angstrom, V = 3064.21 (8) angstrom(3), and Z = 1. The strongest lines of the powder X-ray diffraction pattern [d, angstrom (I, %) (hkl)] are: 11.15 (28) (100), 4.799 (25) (104), 3.973 (16) (105), 3.721 (47) (300), 3.305 (100) (214, 303, 400), 2.661 (17) (008), 2.149 (21) (330). The mineral is named in honour of the outstanding German chemist, a specialist in chemistry of sulfur Prof. Ralf Steudel (1937-2021).
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