chromium-bearing wadsleyite (Cr-Wad) was synthesized in the model system Mg2SiO4– MgCr2O4 at 14 GPa and 1600 °C and studied from the chemical and structural point of views. Microprobe data gave the formula Mg1.930Cr0.120Si0.945O4, on the basis of 4 oxygen atoms. The crystal structure has been studied by single-crystal X-ray diffraction. The orthorhombic unit-cell parameters are: a = 5.6909(5) Å, b = 11.4640(10) Å, c = 8.2406(9) Å, V = 537.62(9) Å3, Z = 8. The structure, space group Imma, was refined to R1 = 5.99% in anisotropic approximation using1135 reflections with Fo > 4σ(Fo) and 43 parameters. Chromium was found to substitute for both Mg at the octahedral sites and Si at the tetrahedral site, according to the reaction VIMg2+ + IVSi4+ = VICr3+ + IVCr3+. On the whole, the structural topology is nearly identical to that of pure wadsleyite. The successful synthesis of Cr-Wad may be important for the thermobarometry of mantle phase associations.
Synthesis and crystal structure of chromium-bearing anhydrous wadsleyite / E. A. Sirotkina, · L. Bindi, A. V. Bobrov, S. M. Aksenov, T. Irifune. - In: PHYSICS AND CHEMISTRY OF MINERALS. - ISSN 0342-1791. - STAMPA. - 45:(2018), pp. 361-366. [10.1007/s00269-017-0926-x]
Synthesis and crystal structure of chromium-bearing anhydrous wadsleyite
· L. BindiMembro del Collaboration Group
;
2018
Abstract
chromium-bearing wadsleyite (Cr-Wad) was synthesized in the model system Mg2SiO4– MgCr2O4 at 14 GPa and 1600 °C and studied from the chemical and structural point of views. Microprobe data gave the formula Mg1.930Cr0.120Si0.945O4, on the basis of 4 oxygen atoms. The crystal structure has been studied by single-crystal X-ray diffraction. The orthorhombic unit-cell parameters are: a = 5.6909(5) Å, b = 11.4640(10) Å, c = 8.2406(9) Å, V = 537.62(9) Å3, Z = 8. The structure, space group Imma, was refined to R1 = 5.99% in anisotropic approximation using1135 reflections with Fo > 4σ(Fo) and 43 parameters. Chromium was found to substitute for both Mg at the octahedral sites and Si at the tetrahedral site, according to the reaction VIMg2+ + IVSi4+ = VICr3+ + IVCr3+. On the whole, the structural topology is nearly identical to that of pure wadsleyite. The successful synthesis of Cr-Wad may be important for the thermobarometry of mantle phase associations.| File | Dimensione | Formato | |
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