Abstract
Tistarite, ideally Ti2O3, is a new member of the corundum-hematite group. It is found as one subhedral crystal in a cluster of micrometer-sized refractory grains along with khamrabaevite (TiC), rutile, and corundum crystals within a chondrule from the Allende meteorite. The mean chemical composition determined by electron microprobe analysis is (wt%) Ti2O3 94.94, MgO 2.06, Al2O3 1.50, ZrO2 0.44, FeO 0.24, CaO 0.10, Cr2O3 0.06, sum 99.34. The empirical formula calculated on the basis of 3 O atoms is (Ti3+ 1.90Mg0.07Al0.04Zr0.01)Σ2.02O3. Tistarite is rhombohedral, R3̄c; a = 5.158 Å, c = 13.611 Å, V = 313.61 Å3, and Z = 6. Its electron back-scatter diffraction pattern matches that of synthetic Ti2O3 with the R3̄c structure. The strongest calculated X-ray powder diffraction lines from the synthetic Ti2O3 data are [d spacing in Å (I) hkl]: 3.734 (84) (012), 2.707 (88) (104), 2.579 (90) (110), 2.242 (38) (113), 1.867 (33) (024), 1.703 (100) (116), 1.512 (28) (214), 1.489 (46) (300), 1.121 (20) (226), 0.896 (25) (416). The mineral is named after the composition “Ti” and the word “star,” implying that this new refractory mineral is among the first solids formed in the solar system.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- Closure temperatures of intracrystalline ordering in anatectic and metamorphic hercynite, Fe2+Al2O4
- Arsenate substitution in hydroxylapatite: Structural characterization of the Ca5(PxAs1–xO4)3OH solid solution
- The crystal chemical role of Zn in alunite-type minerals: Structure refinements for kintoreite and zincian kintoreite
- Application of precession electron diffraction to the characterization of (021) twinning in pseudo-hexagonal coesite
- Structure, thermodynamic, and transport properties of molten Mg2SiO4: Molecular dynamics simulations and model EOS
- High-pressure behavior of åkermanite and gehlenite and phase stability of the normal structure in melilites
- Synchrotron-based speciation of chromium in an Oxisol from New Caledonia: Importance of secondary Fe-oxyhydroxides
- Meurigite-Na, a new species, and the relationship between phosphofibrite and meurigite
- The role of silver on the stabilization of the incommensurately modulated structure in calaverite, AuTe2
- Hydrogen zoning in zinc-bearing staurolite from a high-P, low-T diasporite (Samos, Greece): A combined EMP-SIMS-FIB-FTIR study
- Dmitryivanovite: A new high-pressure calcium aluminum oxide from the Northwest Africa 470 CH3 chondrite characterized using electron backscatter diffraction analysis
- Crystal chemistry of hydrous forsterite and its vibrational properties up to 41 GPa
- The geothermobarometric potential of tourmaline, based on experimental and natural data
- Inverse spinel structure of Co-doped gahnite
- Advances in understanding the structure of borosilicate glasses: A Raman spectroscopy study
- The occurrence of tetrahedrally coordinated Al and B in tourmaline: An 11B and 27Al MAS NMR study
- Accurate and precise lattice parameters by selected-area electron diffraction in the transmission electron microscope
- Two types of metamorphic monazite with contrasting La/Nd, Th, and Y signatures in an ultrahigh-pressure metapelite from the Pohorje Mountains, Slovenia: Indications for pressure-dependent REE exchange between apatite and monazite?
- Cs-exchange in birnessite: Reaction mechanisms inferred from time-resolved X-ray diffraction and transmission electron microscopy
- Crystal chemistry and radiation-induced amorphization of P-coffinite from the natural fission reactor at Bangombé, Gabon
- Letter. Tistarite, Ti2O3, a new refractory mineral from the Allende meteorite
- Letter. Davisite, CaScAlSiO6, a new pyroxene from the Allende meteorite
- Letter. The 4500 cm–1 infrared absorption band in hydrous aluminosilicate glasses is a combination band of the fundamental (Si,Al)-OH and O-H vibrations
Articles in the same Issue
- Closure temperatures of intracrystalline ordering in anatectic and metamorphic hercynite, Fe2+Al2O4
- Arsenate substitution in hydroxylapatite: Structural characterization of the Ca5(PxAs1–xO4)3OH solid solution
- The crystal chemical role of Zn in alunite-type minerals: Structure refinements for kintoreite and zincian kintoreite
- Application of precession electron diffraction to the characterization of (021) twinning in pseudo-hexagonal coesite
- Structure, thermodynamic, and transport properties of molten Mg2SiO4: Molecular dynamics simulations and model EOS
- High-pressure behavior of åkermanite and gehlenite and phase stability of the normal structure in melilites
- Synchrotron-based speciation of chromium in an Oxisol from New Caledonia: Importance of secondary Fe-oxyhydroxides
- Meurigite-Na, a new species, and the relationship between phosphofibrite and meurigite
- The role of silver on the stabilization of the incommensurately modulated structure in calaverite, AuTe2
- Hydrogen zoning in zinc-bearing staurolite from a high-P, low-T diasporite (Samos, Greece): A combined EMP-SIMS-FIB-FTIR study
- Dmitryivanovite: A new high-pressure calcium aluminum oxide from the Northwest Africa 470 CH3 chondrite characterized using electron backscatter diffraction analysis
- Crystal chemistry of hydrous forsterite and its vibrational properties up to 41 GPa
- The geothermobarometric potential of tourmaline, based on experimental and natural data
- Inverse spinel structure of Co-doped gahnite
- Advances in understanding the structure of borosilicate glasses: A Raman spectroscopy study
- The occurrence of tetrahedrally coordinated Al and B in tourmaline: An 11B and 27Al MAS NMR study
- Accurate and precise lattice parameters by selected-area electron diffraction in the transmission electron microscope
- Two types of metamorphic monazite with contrasting La/Nd, Th, and Y signatures in an ultrahigh-pressure metapelite from the Pohorje Mountains, Slovenia: Indications for pressure-dependent REE exchange between apatite and monazite?
- Cs-exchange in birnessite: Reaction mechanisms inferred from time-resolved X-ray diffraction and transmission electron microscopy
- Crystal chemistry and radiation-induced amorphization of P-coffinite from the natural fission reactor at Bangombé, Gabon
- Letter. Tistarite, Ti2O3, a new refractory mineral from the Allende meteorite
- Letter. Davisite, CaScAlSiO6, a new pyroxene from the Allende meteorite
- Letter. The 4500 cm–1 infrared absorption band in hydrous aluminosilicate glasses is a combination band of the fundamental (Si,Al)-OH and O-H vibrations