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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Far East
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Philippine Islands
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Luzon
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Primary terms
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X-ray analysis (4)
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Mossbauer spectroscopy
Equilibrium Fractionation of Non-traditional Isotopes: a Molecular Modeling Perspective
Accurate determination of ferric iron in garnets
Accurate determination of Fe 3+ /∑Fe of andesitic glass by Mössbauer spectroscopy
Mössbauer spectroscopic study of natural eosphorite, [(Mn,Fe)AlPO 4 (OH) 2 H 2 O]
Mössbauer parameters of iron in phosphate minerals: Implications for interpretation of martian data
NQR/NMR and Mössbauer spectroscopy of sulfides: potential and versatility
Accurate determination of ferric iron in garnets by bulk Mössbauer spectroscopy and synchrotron micro-XANES
A semi-quantitative approach to derive the electric field gradient, applied to synthetic fayalite, α -Fe 2 SiO 4 : a reappraisal
In situ monitoring of lepidocrocite bioreduction and magnetite formation by reflection Mössbauer spectroscopy
High-temperature Mössbauer spectroscopy: A probe for the relaxation time of Fe species in silicate melts and glasses
Determination of nanoparticulate magnetite stoichiometry by Mössbauer spectroscopy, acidic dissolution, and powder X-ray diffraction: A critical review
6 th European Conference on Mineralogy and Spectroscopy: Preface
Mössbauer spectroscopy with high velocity resolution in the study of iron-bearing minerals in meteorites
We summarize recent developments of nuclear resonant spectroscopy methods, such as nuclear resonant inelastic X-ray scattering and synchrotron Mössbauer spectroscopy, and their uses for the geophysical sciences. The inelastic method provides specific vibrational information, for example, the phonon density of states, and, in combination with compression data, it permits the determination of sound velocities and Grüneisen parameters under high pressure and high temperature. The Mössbauer method provides hyperfine interactions between the resonant nucleus and electronic environment, such as isomer shifts, quadrupole splittings, and magnetic fields, which provide important information on valence, spin state, and magnetic ordering. Both methods use a nuclear resonant isotope as a probe and can be applied under high pressure and high temperature. The physical mechanism of nuclear resonant scattering and the specifics in applications to Earth materials are presented with reference to several high-pressure studies on iron-bearing compounds.