Mineralogical Magazine · 1972 · 43 citations · 9 references
Natural SciencesChemistryMaterials ScienceCrystal StructureInorganic ChemistrySolid-state ChemistryCrystal ChemistryCrystal LatticeCrystal SymmetryCrystallographyStructure DeterminationX-ray CrystallographyPowder DiffractionPowder Diffraction AnalysisTetragonal Crystal LatticesTetragonal SystemTriclinic SystemUnit Cell DeterminationUnit Cell GeometryUnit Cell Parameters
Summary The structural formula of stilpnomelane averaged from 37 representative literature analyses and based on the determined structure is (Ca,Na,K) 4 (Ti 0·1 Al 2·3 Fe 35·5 Mn 0·8 Mg 9·3 )[Si 63 Al 9 ](O,OH) 216 · n H 2 O. Ferrostilpnomelanes have up to 12 R 3+ cations in the octahedral sheet, ferristilpnomelanes commonly have between 24 and 30 R 3+ cations, rarely up to 37. The two groups can be distinguished by accurate X-ray powder diffraction, ferrostilpnomelanes having d 001 less and a greater than have ferristilpnomelanes. The unit cell is triclinic, a = b ∼21·8 Å, γ = 120°, d 001 ∼12·2 Å, P . Hexagonal groups or ‘islands’ of 24 silicon-oxygen tetrahedra co-ordinate to the octahedral sheet, the centres of the ‘islands’ are displaced by 5 a /12, 8 b /12 on either side of the octahedral sheet as a result of warping of this sheet to permit articulation with the smaller tetrahedral sheet. The 24-tetrahedra ‘islands’ are linked laterally by 6-member rings of inverted tetrahedra, which in turn link at their apices to like rings connecting the next sheet of ‘islands’. Thus a single tetrahedral layer is 4 tetrahedra thick and has symmetry 6/ m . The 6-member rings of tetrahedra act as hinges permitting up to 0·5 Å extension or contraction of the tetrahedral sheet to accommodate variations in the octahedral sheet dimensions with varying R 2+ / R 3+ ratio.
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Iron phyllosilicates of the cuyuna district in Minnesota
R. L. Blake · American Mineralogist · 1965 · 29 citations