American Mineralogist · 2017 · 11 citations · 18 references
Natural SciencesEarth SciencesGeologyCrystal StructureGeochemistryMineralogyCrystal ChemistryMetamorphic MineralsMineral ChemistryMineral GenesisNanomaterial CharacterizationPhysical Properties Of MineralsDiffraction PatternsEnergy-dispersive X-ray SpectroscopyHigh-resolution Electron MicroscopyHigh-resolution Transmission Electron MicroscopyLow-temperature MaterialsNanocrystalsSelected Area Electron DiffractionUnit Cell Parameters
Al-Fe-bearing protoenstatite was discovered in Oregon sunstones with unusual pleochroic/dichroic red to green coloration using high-resolution transmission electron microscopy (HRTEM) and X-ray energy-dispersive spectroscopy (EDS). The empirical formula calculated on the basis of 6 O apfu is (Mg1.17Fe0.43Al0.26Ca0.03Na0.10Ti0.01)Σ2.00(Si1.83Al0.17)Σ2.00O6. The protoenstatite has a space group of Pbcn; its unit-cell parameters refined from selected-area electron diffraction patterns are a = 9.25(1), b = 8.78(1), and c = 5.32(1) Å. Protoenstatite nanocrystals are quenchable to low temperature. The crystallographically oriented nanocrystals of protoenstatite and clinoenstatite in association with copper nanocrystals are responsible for the unusual green and "watermelon" coloration of the labradorite gemstone.
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Structural and chemical variations in pyroxenes
Maryellen Cameron, J. J. Papike · 1981 · 287 citations
Stability of high-density clinoenstatite at upper-mantle pressures
R. J. Angel, A. Chopelas, Nancy L. Ross · Nature · 1992 · 201 citations