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The crystal structure of peprossiite-(Ce), an anhydrous REE and Al mica-like borate with square-pyramidal coordination for Al

  • Athos Callegari , Franca Caucia , Fiorenzo Mazzi , Roberta Oberti EMAIL logo , Luisa Ottolini and Luciano Ungaretti
Published/Copyright: March 26, 2015
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American Mineralogist
From the journal American Mineralogist Volume 85 Issue 3-4

Abstract

Single-crystal structure refinements are presented of the holotype of crystal peprossiite-(Ce) (Monte Cavalluccio) and of a new sample from Cura di Vetralla (Viterbo, Italy) with slightly different composition, together with new EMP-SIMS chemical analyses. These results allow us to propose a new unit formula: [REE1-x-y(Th,U)xCay](Al3O)2/3[(B4-zSiz)]O10 with x - y + z = 1/3 (Z = 1) for the peprossiite group. Lattice constants for the holotype crystal are: a = 4.612(1), c = 9.374(3) Å, V = 172.6 Å3, Z = 1, space group P6̅ 2m. The crystal structure was solved by Patterson methods and refined to Robs = 1.8% (Rall = 2.2%) for 706 unique reflections in the 2q-range 6-136°. Lattice constants for the thorian peprossiite-(Ce) from Cura di Vetralla are: a = 4.596(3), c = 9.309(16) Å, V = 170.3 Å3, and the structure was refined to Robs = 2.9% and Rall = 3.0% for 271 unique reflections in the 2θ-range 4-80°. The topology of the tetrahedral layer and the site of the inter-layer cation (REE) in peprossiite resembles that of dioctahedral micas. The main difference lies in the presence of layers of pyramids instead of layers of octahedra typical of mica. In peprossiite, Al is coordinated by five O atoms in a nearly square-pyramidal arrangement, the base of which is formed by pairs of apical O atoms from two layers of tetrahedra related by a mirror plane. Three of these pyramids share their apical O forming Al3O groups with occupancy of 2/3 according to the structure refinement. A model is proposed that explains the apparent disorder in the pyramidal layer of peprossiite by the stacking within a triple cell (with a′ = a √ 3 and a ^ a′ = 30°) of three ordered layers randomly translated by ± a.

Received: 1999-5-5
Accepted: 1999-11-1
Published Online: 2015-3-26
Published in Print: 2000-4-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Iron concentration and the physical processes of dynamic oxidation in an alkaline earth aluminosilicate glass
  2. A crystal chemical re-evaluation of amphibole/melt and amphibole/clinopyroxene DTi values in petrogenetic studies
  3. Mineralogy of mafic xenoliths and their reaction zones in the olivine lamproite from Prairie Creek Arkansas and the paragenesis of haggertyite, Ba [Fe6Ti5Mg]O19
  4. Magmatic anhydrite in granitic rocks: First occurrence and potential petrologic consequences
  5. Crystal chemistry of Al-rich biotites coexisting with muscovites in peraluminous granites
  6. Spectroscopic and structural properties of synthetic micas on the annite-siderophyllite binary: Synthesis, crystal structure refinement, Mössbauer, and infrared spectroscopy
  7. Thermodynamic properties of tremolite: A correction and some comments
  8. Raman spectroscopic characteristics of Mg-Fe-Ca pyroxenes
  9. Hydrogen in diopside: Diffusion profiles
  10. Diffusion of C and O in calcite at 100 MPa
  11. Solubility and stability of zeolites in aqueous solution: II. Calcic clinoptilolite and mordenite
  12. TEM and SFM of exsolution and twinning in an alkali feldspar
  13. Equation of state of magnetite and its high-pressure modification: Thermodynamics of the Fe-O system at high pressure
  14. Optimization of site occupancies in minerals using quadratic programming
  15. Leverage analysis and structure refinement of minerals
  16. The absolute energy positions of conduction and valence bands of selected semiconducting minerals
  17. Antiferroelectric phase transition in titanite: Excess entropy and short range order
  18. P4/n and P4nc long-range ordering in low-temperature vesuvianites
  19. Tetrahedral vacancies and cation ordering in low-temperature Mn-bearing vesuvianites: Indication of a hydrogarnet-like substitution
  20. Sodic-ferripedrizite, a new monoclinic amphibole bridging the magnesium-iron-manganese-lithium and the sodium-calcium groups
  21. The crystal structure of peprossiite-(Ce), an anhydrous REE and Al mica-like borate with square-pyramidal coordination for Al
  22. Crystal chemistry of the new mineral brandholzite, Mg(H2O)6[Sb(OH)6]2, and of the synthetic analogues M2+(H2O)6[Sb(OH)6]2 (M2+ = Mg, Co)
  23. Letters. In-situ Raman spectra of dissolved silica species in aqueous fluids to 900 °C and 14 kbar
  24. Quetzalcoatlite: A new octahedral-tetrahedral structure from a 2 × 2 × 40 μm3 crystal at the Advanced Photon Source-GSE-CARS Facility
  25. Bonding and dynamics of Mg in pyrope: a theoretical investigation
  26. Structure of a new Al-rich phase, [K, Na]0.9[Mg, Fe]2[Mg, Fe, Al, Si]6O12, synthesized at 24 GPa
  27. Core level electron binding energies of realgar (As4S4)
  28. Oxidation of {100} and {111} surfaces of pyrite: Effects of preparation method
https://doi.org/10.2138/am-2000-0421

Articles in the same Issue

  1. Iron concentration and the physical processes of dynamic oxidation in an alkaline earth aluminosilicate glass
  2. A crystal chemical re-evaluation of amphibole/melt and amphibole/clinopyroxene DTi values in petrogenetic studies
  3. Mineralogy of mafic xenoliths and their reaction zones in the olivine lamproite from Prairie Creek Arkansas and the paragenesis of haggertyite, Ba [Fe6Ti5Mg]O19
  4. Magmatic anhydrite in granitic rocks: First occurrence and potential petrologic consequences
  5. Crystal chemistry of Al-rich biotites coexisting with muscovites in peraluminous granites
  6. Spectroscopic and structural properties of synthetic micas on the annite-siderophyllite binary: Synthesis, crystal structure refinement, Mössbauer, and infrared spectroscopy
  7. Thermodynamic properties of tremolite: A correction and some comments
  8. Raman spectroscopic characteristics of Mg-Fe-Ca pyroxenes
  9. Hydrogen in diopside: Diffusion profiles
  10. Diffusion of C and O in calcite at 100 MPa
  11. Solubility and stability of zeolites in aqueous solution: II. Calcic clinoptilolite and mordenite
  12. TEM and SFM of exsolution and twinning in an alkali feldspar
  13. Equation of state of magnetite and its high-pressure modification: Thermodynamics of the Fe-O system at high pressure
  14. Optimization of site occupancies in minerals using quadratic programming
  15. Leverage analysis and structure refinement of minerals
  16. The absolute energy positions of conduction and valence bands of selected semiconducting minerals
  17. Antiferroelectric phase transition in titanite: Excess entropy and short range order
  18. P4/n and P4nc long-range ordering in low-temperature vesuvianites
  19. Tetrahedral vacancies and cation ordering in low-temperature Mn-bearing vesuvianites: Indication of a hydrogarnet-like substitution
  20. Sodic-ferripedrizite, a new monoclinic amphibole bridging the magnesium-iron-manganese-lithium and the sodium-calcium groups
  21. The crystal structure of peprossiite-(Ce), an anhydrous REE and Al mica-like borate with square-pyramidal coordination for Al
  22. Crystal chemistry of the new mineral brandholzite, Mg(H2O)6[Sb(OH)6]2, and of the synthetic analogues M2+(H2O)6[Sb(OH)6]2 (M2+ = Mg, Co)
  23. Letters. In-situ Raman spectra of dissolved silica species in aqueous fluids to 900 °C and 14 kbar
  24. Quetzalcoatlite: A new octahedral-tetrahedral structure from a 2 × 2 × 40 μm3 crystal at the Advanced Photon Source-GSE-CARS Facility
  25. Bonding and dynamics of Mg in pyrope: a theoretical investigation
  26. Structure of a new Al-rich phase, [K, Na]0.9[Mg, Fe]2[Mg, Fe, Al, Si]6O12, synthesized at 24 GPa
  27. Core level electron binding energies of realgar (As4S4)
  28. Oxidation of {100} and {111} surfaces of pyrite: Effects of preparation method
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