Symmetry and crystal structure of biaxial elbaite-liddicoatite tourmaline from the Transbaikalia region, Russia
-
Alexander Shtukenberg
, Ira Rozhdestvenskaya
Abstract
Optical anomalies and crystal structures have been studied for an elbaite-liddicoatite tourmaline specimen from the Malkhan pegmatite field (Transbaikalia region, Russia). The specimen is characterized by a complicated zoning and sector zoning distribution of anomalous biaxiality, with the axial angle 2V increasing from 3 up to 23° going from the first to the last growth zones of the most developed growth sector, o{022̅1}. The crystal structures of three samples cut out from different growth zones of that sector and characterized by the axial angles 11, 16, and 23° were refined in the trigonal space group R3m as well as in its monoclinic and triclinic subgroups Cm, R1, and P1, respectively (R = 0.019-0.039). The final choice of the low symmetry space group R1 is based on the analysis of the diffraction patterns and on the results of crystal structures refinements, which revealed ordered Al/Li distributions over the Y octahedral sites. The degree of order at Y sites correlates with the axial angle 2V, which implies a causal relationship. The Al/Li ordering reflects the geometrical differences of the octahedral sites with respect to the growth front orientation. The results obtained suggest that a growth dissymmetrization mechanism is the main reason for the observed cation ordering and optical anomalies.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- New constraints on metamorphic history of Adirondack diopsides (New York, U.S.A.): Al and δ18O profiles
- Hammadah al Hamra 193: The first amphibole-bearing winonaite
- Crystal chemistry of trioctahedral micas in alkaline and subalkaline volcanic rocks: A case study from Mt. Sassetto (Tolfa district, Latium, central Italy)
- Magnetic excitations and heat capacity of fayalite, Fe2SiO4
- The barometer tremolite + tschermakite + 2 albite = 2 pargasite + 8 quartz: Constraints from experimental data at unit silica activity, with application to garnet-free natural assemblages
- In-situ measurement of dissolution of anorthite in Na-Cl-OH solutions at 22 °C using phase-shift interferometry
- Experimental investigation of the breakdown of dolomite in rock cores at 100 MPa, 650-750 °C
- Dissolution of the (001) surface of galena: An in situ assessment of surface speciation by fluid-cell micro-Raman spectroscopy
- An infrared spectroscopic study of the OH stretching frequencies of talc and 10-Å phase to 10 GPa
- Co2+-Cu2+ substitution in bieberite solid-solution series, (Co1-xCux)SO4·7H2O, 0.00 ≤ x ≤ 0.46: Synthesis, single-crystal structure analysis, and optical spectroscopy
- Clinoenstatite exsolution in diopsidic augite of Dabieshan: Garnet peridotite from depth of 300 km
- Heat-pulse calorimetry measurements on natural chlorite-group minerals
- Low-temperature behavior of NaGaSi2O6
- Single-crystal elasticity of zoisite Ca2Al3Si3O12(OH) by Brillouin scattering
- The effect of valence state and site geometry on Ti L3,2 and O K electron energy-loss spectra of TixOy phases
- Characterization of defects and the local structure in natural and synthetic alunite (K, Na, H3O)Al3(SO4)2(OH)6 by multi-nuclear solid-state NMR spectroscopy
- Using a mineral lifetime diagram to evaluate the persistence of olivine on Mars
- Complexity in 15- and 30-sectors polygonal serpentine: Longitudinal sections, intrasector stacking faults and XRPD satellites
- Light-induced alteration of arsenic sulfides: A new product with an orthorhombic crystal structure
- Transmission electron microscopy study of magnetites in a freshwater population of magnetotactic bacteria
- Anomalous behavior at the I2/a to Imab phase transition in SiO2-moganite: An analysis using hard-mode Raman spectroscopy
- The system Ag-Au-Se: Phase relations below 405 K and determination of standard thermodynamic properties of selenides by solid-state galvanic cell technique
- Rhombohedral (9R) and hexagonal (6H) perovskites in barium silicates under high pressure
- Structural effects of pressure on monoclinic chlorite: A single-crystal study
- Neptunium incorporation in sodium-substituted metaschoepite
- The effect of H2O on olivine crystallization in MORB: Experimental calibration at 200 MPa
- Symmetry and crystal structure of biaxial elbaite-liddicoatite tourmaline from the Transbaikalia region, Russia
- Letter: Onion morphology and microstructure of polyhedral serpentine
- Letter: Ion microprobe analysis of (231Pa)/(235U) and an appraisal of protactinium partitioning in igneous zircon
- Letter: Structural investigation of Mg local environments in silicate glasses by ultra-high field 25Mg 3QMAS NMR spectroscopy
- Letter: Entropies of mixing and subsolidus phase relations of forsteritefayalite (Mg2SiO4Fe2SiO4) solid solution
Articles in the same Issue
- New constraints on metamorphic history of Adirondack diopsides (New York, U.S.A.): Al and δ18O profiles
- Hammadah al Hamra 193: The first amphibole-bearing winonaite
- Crystal chemistry of trioctahedral micas in alkaline and subalkaline volcanic rocks: A case study from Mt. Sassetto (Tolfa district, Latium, central Italy)
- Magnetic excitations and heat capacity of fayalite, Fe2SiO4
- The barometer tremolite + tschermakite + 2 albite = 2 pargasite + 8 quartz: Constraints from experimental data at unit silica activity, with application to garnet-free natural assemblages
- In-situ measurement of dissolution of anorthite in Na-Cl-OH solutions at 22 °C using phase-shift interferometry
- Experimental investigation of the breakdown of dolomite in rock cores at 100 MPa, 650-750 °C
- Dissolution of the (001) surface of galena: An in situ assessment of surface speciation by fluid-cell micro-Raman spectroscopy
- An infrared spectroscopic study of the OH stretching frequencies of talc and 10-Å phase to 10 GPa
- Co2+-Cu2+ substitution in bieberite solid-solution series, (Co1-xCux)SO4·7H2O, 0.00 ≤ x ≤ 0.46: Synthesis, single-crystal structure analysis, and optical spectroscopy
- Clinoenstatite exsolution in diopsidic augite of Dabieshan: Garnet peridotite from depth of 300 km
- Heat-pulse calorimetry measurements on natural chlorite-group minerals
- Low-temperature behavior of NaGaSi2O6
- Single-crystal elasticity of zoisite Ca2Al3Si3O12(OH) by Brillouin scattering
- The effect of valence state and site geometry on Ti L3,2 and O K electron energy-loss spectra of TixOy phases
- Characterization of defects and the local structure in natural and synthetic alunite (K, Na, H3O)Al3(SO4)2(OH)6 by multi-nuclear solid-state NMR spectroscopy
- Using a mineral lifetime diagram to evaluate the persistence of olivine on Mars
- Complexity in 15- and 30-sectors polygonal serpentine: Longitudinal sections, intrasector stacking faults and XRPD satellites
- Light-induced alteration of arsenic sulfides: A new product with an orthorhombic crystal structure
- Transmission electron microscopy study of magnetites in a freshwater population of magnetotactic bacteria
- Anomalous behavior at the I2/a to Imab phase transition in SiO2-moganite: An analysis using hard-mode Raman spectroscopy
- The system Ag-Au-Se: Phase relations below 405 K and determination of standard thermodynamic properties of selenides by solid-state galvanic cell technique
- Rhombohedral (9R) and hexagonal (6H) perovskites in barium silicates under high pressure
- Structural effects of pressure on monoclinic chlorite: A single-crystal study
- Neptunium incorporation in sodium-substituted metaschoepite
- The effect of H2O on olivine crystallization in MORB: Experimental calibration at 200 MPa
- Symmetry and crystal structure of biaxial elbaite-liddicoatite tourmaline from the Transbaikalia region, Russia
- Letter: Onion morphology and microstructure of polyhedral serpentine
- Letter: Ion microprobe analysis of (231Pa)/(235U) and an appraisal of protactinium partitioning in igneous zircon
- Letter: Structural investigation of Mg local environments in silicate glasses by ultra-high field 25Mg 3QMAS NMR spectroscopy
- Letter: Entropies of mixing and subsolidus phase relations of forsteritefayalite (Mg2SiO4Fe2SiO4) solid solution