The phosphate mineral sigloite Fe3+Al2(PO4)2(OH)3·7(H2O), an exception to the paragenesis rule – A vibrational spectroscopic study

Ray L. Frost; Yunfei Xi; Ricardo Scholz; Fernanda Maria Belotti; Mauro Cândido Filho

doi:10.1016/j.molstruc.2012.10.020

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The phosphate mineral sigloite Fe3+Al2(PO4)2(OH)3·7(H2O), an exception to the paragenesis rule – A vibrational spectroscopic study

Ray L. Frost Yunfei Xi Ricardo Scholz Fernanda Maria Belotti Mauro Cândido Filho

Year: 2012 Journal: Journal of Molecular Structure Vol: 1033 Pages: 258-264 Publisher: Elsevier BV

DOI: 10.1016/j.molstruc.2012.10.020

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Keywords:

Chemistry Phosphate minerals Raman spectroscopy Paragenesis Phosphate Mineral Analytical Chemistry (journal) Infrared spectroscopy Crystallography Mineralogy Metallurgy Materials science

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Clay minerals and soil interactions

Physical Sciences → Materials Science → Biomaterials

Crystal Structures and Properties

Physical Sciences → Materials Science → Electronic, Optical and Magnetic Materials

Iron oxide chemistry and applications

Physical Sciences → Energy → Renewable Energy, Sustainability and the Environment

The phosphate mineral sigloite Fe3+Al2(PO4)2(OH)3·7(H2O), an exception to the paragenesis rule – A vibrational spectroscopic study

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