Browsing ELibrary by Author "Quartieri S."
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Browsing ELibrary by Author "Quartieri S."
Now showing items 1-7 of 7
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Quartieri S.; Dalconi M.C.; Boscherini F.; Oberti R.; D'Acapito F. (2004)The site location and local geometry of trace amounts (299 ppm) of dysprosium in a natural melanite garnet from a carbonatitic rock have been studied by high-energy fluorescence-detected X-ray absorption fine-structure ...
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Quartieri S.; Boscherini F.; Chaboy J.; Dalconi M.C.; Oberti R.; Zanetti A. (2002)Natural melanite garnets from carbonatitic rocks have been studied by a multitechnique approach based on both experimental (chemical, diffractometric and spectroscopic) methods and full-multiple scattering calculations of ...
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Ferro O.; Vezzalini G.; Quartieri S.; Ceriani C.; Fois E.; Gamba A.; Cruciani G. (2004)The thermal dehydration process of the natural Li zeolite bikitaite has been studied in situ by synchrotron radiation powder diffraction. The temperature-resolved experiments were performed using a translating imaging plate ...
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Sani A.; Quartieri S.; Boscherini F.; Antonioli G.; Feenstra A.; Geiger C.A. (2004)X-ray absorption fine structure (XAFS) measurements at the Fe and Mn K-edges were undertaken to investigate the Fe2+-O and Mn2+-O bonding, and Fe2+- and Mn2+-vibrational properties for a series of synthetic almandine-spessartine, ...
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Ferro O.; Quartieri S.; Vezzalini G.; Fois E.; Gamba A.; Tabacchi G. (2002)Pressure-induced structural modifications in the zeolite bikitaite are studied by means of in situ synchrotron X-ray powder diffraction and ab initio molecular dynamics. The experimental cell parameters were refined up to ...
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Ballone P.; Quartieri S.; Sani A.; Vezzalini G. (2002)Pressure-induced structural modifications in scolecite were studied by means of in situ synchrotron X-ray powder diffraction and density functional computations. The experimental cell parameters were refined up to 8.5 GPa. ...
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Arletti R.; Ferro O.; Vezzalini G.; Quartieri S.; Sani A.; Tabacchi G. (2003)The HP behavior of the natural zeolite yugawaralite and of the synthetic zeolite Na-A was studied by in situ synchrotron X-ray powder diffraction, using a non-penetrating P-transmitting medium. The unit-cell parameters of ...
Now showing items 1-7 of 7
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