High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel. / Nestola, F.; Balic Zunic, Tonci; Koch-Müller, M.; Secco, L.; Princivalle, F.; Parisi, F.; Negro, A. Dal.

In: Mineralogical Magazine, Vol. 75, No. 5, 2011, p. 2649–2655.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Nestola, F, Balic Zunic, T, Koch-Müller, M, Secco, L, Princivalle, F, Parisi, F & Negro, AD 2011, 'High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel', Mineralogical Magazine, vol. 75, no. 5, pp. 2649–2655. https://doi.org/10.1180/minmag.2011.075.5.2649

APA

Nestola, F., Balic Zunic, T., Koch-Müller, M., Secco, L., Princivalle, F., Parisi, F., & Negro, A. D. (2011). High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel. Mineralogical Magazine, 75(5), 2649–2655. https://doi.org/10.1180/minmag.2011.075.5.2649

Vancouver

Nestola F, Balic Zunic T, Koch-Müller M, Secco L, Princivalle F, Parisi F et al. High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel. Mineralogical Magazine. 2011;75(5):2649–2655. https://doi.org/10.1180/minmag.2011.075.5.2649

Author

Nestola, F. ; Balic Zunic, Tonci ; Koch-Müller, M. ; Secco, L. ; Princivalle, F. ; Parisi, F. ; Negro, A. Dal. / High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel. In: Mineralogical Magazine. 2011 ; Vol. 75, No. 5. pp. 2649–2655.

Bibtex

@article{a3b06295652c4efe8b5477a40de1beea,
title = "High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel",
abstract = "The crystal structure of Fe2SiO4 spinel at room temperature was investigated at seven different pressures by X-ray diffraction, using a diamond anvil cell to examine the influence of Fe substitution on ringwoodite behaviour at high pressure. The results compared with those of a pure Mg endmember show that the substitution of Fe into the spinel structure causes only small changes in the compression rate of coordination polyhedra and the distortion of the octahedron. The data show that the compression rate for the octahedron and tetrahedron in (Mg,Fe)2SiO4 can be considered statistically equal for FeO6 and MgO6, as well as for SiO4 in both the endmembers. This shows why almost identical bulk moduli are reported along the solid solution in recent literature.",
author = "F. Nestola and {Balic Zunic}, Tonci and M. Koch-M{\"u}ller and L. Secco and F. Princivalle and F. Parisi and Negro, {A. Dal}",
year = "2011",
doi = "10.1180/minmag.2011.075.5.2649",
language = "English",
volume = "75",
pages = "2649–2655",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
number = "5",

}

RIS

TY - JOUR

T1 - High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel

AU - Nestola, F.

AU - Balic Zunic, Tonci

AU - Koch-Müller, M.

AU - Secco, L.

AU - Princivalle, F.

AU - Parisi, F.

AU - Negro, A. Dal

PY - 2011

Y1 - 2011

N2 - The crystal structure of Fe2SiO4 spinel at room temperature was investigated at seven different pressures by X-ray diffraction, using a diamond anvil cell to examine the influence of Fe substitution on ringwoodite behaviour at high pressure. The results compared with those of a pure Mg endmember show that the substitution of Fe into the spinel structure causes only small changes in the compression rate of coordination polyhedra and the distortion of the octahedron. The data show that the compression rate for the octahedron and tetrahedron in (Mg,Fe)2SiO4 can be considered statistically equal for FeO6 and MgO6, as well as for SiO4 in both the endmembers. This shows why almost identical bulk moduli are reported along the solid solution in recent literature.

AB - The crystal structure of Fe2SiO4 spinel at room temperature was investigated at seven different pressures by X-ray diffraction, using a diamond anvil cell to examine the influence of Fe substitution on ringwoodite behaviour at high pressure. The results compared with those of a pure Mg endmember show that the substitution of Fe into the spinel structure causes only small changes in the compression rate of coordination polyhedra and the distortion of the octahedron. The data show that the compression rate for the octahedron and tetrahedron in (Mg,Fe)2SiO4 can be considered statistically equal for FeO6 and MgO6, as well as for SiO4 in both the endmembers. This shows why almost identical bulk moduli are reported along the solid solution in recent literature.

U2 - 10.1180/minmag.2011.075.5.2649

DO - 10.1180/minmag.2011.075.5.2649

M3 - Journal article

VL - 75

SP - 2649

EP - 2655

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

IS - 5

ER -

ID: 49593038