Magnetic Vortex States in Small Octahedral Particles of Intermediate Titanomagnetite

Abstract Fine particles of titanomagnetites (Fe3‐xTixO4, x > 0.5) in the pseudo‐single‐domain (PSD) size (0.5–20 μm) are important carriers of natural remanent magnetization in basalts. Understanding the mechanism of magnetic recording in these grains has important implications for paleomagnetic...

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Bibliographic Details
Main Authors: E. Khakhalova, B. M. Moskowitz, W. Williams, A. R. Biedermann, P. Solheid
Format: Article
Language:English
Published: Wiley 2018-09-01
Series:Geochemistry, Geophysics, Geosystems
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Online Access:https://doi.org/10.1029/2018GC007723
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