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López-Sánchez, J., McIntosh, G., Osete, M. L., del Campo, A., Villalaín, J. J., Pérez, L., Kovacheva, M., Rodríguez de la Fuente, O. (2017) Epsilon iron oxide: Origin of the high coercivity stable low Curie temperature magnetic phase found in heated archeological materials. Geochemistry, Geophysics, Geosystems, 18 (7) 2646-2656 doi:10.1002/2017gc006929

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Reference TypeJournal (article/letter/editorial)
TitleEpsilon iron oxide: Origin of the high coercivity stable low Curie temperature magnetic phase found in heated archeological materials
JournalGeochemistry, Geophysics, Geosystems
AuthorsLópez-Sánchez, J.Author
McIntosh, G.Author
Osete, M. L.Author
del Campo, A.Author
Villalaín, J. J.Author
Pérez, L.Author
Kovacheva, M.Author
Rodríguez de la Fuente, O.Author
Year2017 (July)Volume18
Issue7
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1002/2017gc006929Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID407609Long-form Identifiermindat:1:5:407609:8
GUID0
Full ReferenceLópez-Sánchez, J., McIntosh, G., Osete, M. L., del Campo, A., Villalaín, J. J., Pérez, L., Kovacheva, M., Rodríguez de la Fuente, O. (2017) Epsilon iron oxide: Origin of the high coercivity stable low Curie temperature magnetic phase found in heated archeological materials. Geochemistry, Geophysics, Geosystems, 18 (7) 2646-2656 doi:10.1002/2017gc006929
Plain TextLópez-Sánchez, J., McIntosh, G., Osete, M. L., del Campo, A., Villalaín, J. J., Pérez, L., Kovacheva, M., Rodríguez de la Fuente, O. (2017) Epsilon iron oxide: Origin of the high coercivity stable low Curie temperature magnetic phase found in heated archeological materials. Geochemistry, Geophysics, Geosystems, 18 (7) 2646-2656 doi:10.1002/2017gc006929
In(2017, July) Geochemistry, Geophysics, Geosystems Vol. 18 (7) American Geophysical Union (AGU)


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