Abstract
Davisite, ideally CaScAlSiO6, is a new member of the Ca clinopyroxene group, where Sc3+ is dominant in the M1 site. It occurs as micro-sized crystals along with perovskite and spinel in an ultra-refractory inclusion from the Allende meteorite. The mean chemical composition determined by electron microprobe analysis is (wt%) SiO2 26.24, CaO 23.55, Al2O3 21.05, Sc2O3 14.70, TiO2 (total) 8.66, MgO 2.82, ZrO2 2.00, Y2O3 0.56, V2O3 0.55, FeO 0.30, Dy2O3 0.27, Gd2O3 0.13, Er2O3 0.08, sum 100.91. Its empirical formula calculated on the basis of 6 O atoms is Ca0.99(Sc0.50Ti3+0.16Mg0.16Ti4+0.10 Zr0.04V3+0.02Fe2+0.01Y0.01)Σ1.00(Si1.03Al0.97) Σ2.00O6. Davisite is monoclinic, C2/c; a = 9.884 Å, b = 8.988 Å, c = 5.446 Å, β =105.86°, V = 465.39 Å3, and Z = 4. Its electron back-scattered diffraction pattern is an excellent match to that of synthetic CaScAlSiO6 with the C2/c structure. The strongest calculated X-ray powder diffraction lines are [d spacing in Å (I) (hkl)]: 3.039 (100) (2̄21), 2.989 (31) (310), 2.943 (18) (3̄11), 2.619 (40) (002), 2.600 (26) (1̄31), 2.564 (47) (221), 2.159 (18) (3̄31), 2.137 (15) (4̄21), 1.676 (20) (2̄23), and 1.444 (18) (531). The name is for Andrew M. Davis, a cosmochemist at the University of Chicago, Illinois.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- Closure temperatures of intracrystalline ordering in anatectic and metamorphic hercynite, Fe2+Al2O4
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- 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
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- The role of silver on the stabilization of the incommensurately modulated structure in calaverite, AuTe2
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- 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