Epsilon iron oxide: Origin of the high coercivity stable low <scp>C</scp>urie temperature magnetic phase found in heated archeological materials
2017 · Geochemistry Geophysics Geosystems · 58 citations
https://doi.org/10.1002/2017gc006929
G
G. McIntosh
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51
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23
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G. McIntosh is an academic researcher from Canterbury Christ Church University. The author has contributed to research in topics: Geomagnetism and Paleomagnetism Studies & Geology and Paleoclimatology Research & Geophysical and Geoelectrical Methods. The author has an h-index of 19, co-authored 44 publications.
ORCID: 0000-0002-1635-2217Papers by this author
worksWidespread occurrence of a novel high coercivity, thermally stable, low unblocking temperature magnetic phase in heated archeological material
2007 · Geophysical Research Letters · 43 citations
https://doi.org/10.1029/2007gl031168
High coercivity remanence in baked clay materials used in archeomagnetism
2011 · Geochemistry Geophysics Geosystems · 37 citations
https://doi.org/10.1029/2010gc003310
Further progress in the study of epsilon iron oxide in archaeological baked clays
2020 · Physics of The Earth and Planetary Interiors · 25 citations
https://doi.org/10.1016/j.pepi.2020.106554
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