Low-temperature and high-temperature hysteresis of small multidomain magnetites (215–540 nm)

Author:

Argyle Kenneth S.,Dunlop David J.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference87 articles.

1. Magnetic properties of uniform spherical magnetite particles prepared from ferrous hydroxide gels;Amin;Phys. Stat. Solidi A,1987

2. Experimental and theoretical magnetic properties of magnetite in the lower pseudo-single domain particle size range;Argyle,1984

3. Theoretical domain structure in multidomain magnetite particles;Argyle;Geophys. Res. Lett.,1984

4. Alternating field characteristics of pseudo-single-domain (2–14 μm) and multidomain magnetite;Bailey;Earth Planet. Sci. Lett.,1983

5. On the origin of stable remanence in pseudo-single domain grains;Banerjee;J. Geomagn. Geoelectr.,1977

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