Abstract
The structural environment of substitutional Cr3+ ion in a natural pyrope Mg3Al2Si3O12 has been investigated by Cr K-edge extended X-ray absorption fine structure (EXAFS) and X-ray absorption near edge structure (XANES) coupled with first-principles computations. The Cr-O distance is close to that in knorringite Mg3Cr2Si3O12, indicating a nearly full relaxation of the first neighbors. The local C3i symmetry of the octahedral Y site is retained during Cr-Al substitution. The second and third shells of neighbors (Mg and Si) relax only partially. Site relaxation is accommodated by strain-induced bond buckling, with angular tilts of the Si-centered tetrahedra around the Cr-centered octahedron, and by a deformation of the Mg-centered dodecahedra.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- The crystal structure of vurroite, Pb20Sn2(Bi,As)22S54Cl6: OD-character, polytypism, twinning, and modular description
- Mineralogy of the Paso Robles soils on Mars
- Dingdaohengite-(Ce) from the Bayan Obo REE-Nb-Fe Mine, China: Both a true polymorph of perrierite-(Ce) and a titanic analog at the C1 site of chevkinite subgroup
- Thermal equation of state of CaGeO3 perovskite
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- Quantitative absorbance spectroscopy with unpolarized light: Part II. Experimental evaluation and development of a protocol for quantitative analysis of mineral IR spectra
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- Precise dating of biotite in distal volcanic ash: Isolating subtle alteration using 40Ar/39Ar laser incremental heating and electron microprobe techniques
- Rationale for the existence of four- and eight-reversals in antigorite
- Structural relaxation around substitutional Cr3+ in pyrope garnet
- Metasomatic thorite and uraninite inclusions in xenotime and monazite from granitic pegmatites, Hidra anorthosite massif, southwestern Norway: Mechanics and fluid chemistry
- Interlayer potassium and its neighboring atoms in micas: Crystal-chemical modeling and XANES spectroscopy
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- Birchite, a new mineral from Broken Hill, New South Wales, Australia: Description and structure refinement
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- Evidence for anomalously large degree of polymerization in Mg2SiO4 glass and melt
- Theoretical infrared absorption coefficient of OH groups in minerals