Origin of self-reversed thermoremanent magnetization

The ability of certain magnetic minerals to acquire a remanent magnetization that opposes the direction of the Earth's magnetic field has fascinated rock magnetists since its discovery in 1951. Here, we determine the origin of this phenomenon, which is termed self-reversed thermoremanent magnet...

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Veröffentlicht in:Physical review letters 2005-12, Vol.95 (26), p.268501.1-268501.4, Article 268501
Hauptverfasser: HARRISON, Richard J, KASAMA, Takeshi, WHITE, Thomas A, SIMPSON, Edward T, DUNIN-BORKOWSKI, Rafal E
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container_end_page 268501.4
container_issue 26
container_start_page 268501.1
container_title Physical review letters
container_volume 95
creator HARRISON, Richard J
KASAMA, Takeshi
WHITE, Thomas A
SIMPSON, Edward T
DUNIN-BORKOWSKI, Rafal E
description The ability of certain magnetic minerals to acquire a remanent magnetization that opposes the direction of the Earth's magnetic field has fascinated rock magnetists since its discovery in 1951. Here, we determine the origin of this phenomenon, which is termed self-reversed thermoremanent magnetization (SR-TRM). We present direct transmission electron microscopy observations of negative exchange coupling across antiphase domain boundaries (APBs) in ilmenite-hematite. This coupling is linked intrinsically to the origin of SR-TRM and is responsible for the formation of two new classes of magnetic domain wall at APBs. We present simulations of the chemical and magnetic structure of the APBs and show that SR-TRM is generated by coupling between strongly ferrimagnetic Ti-rich domains and weakly ferrimagnetic Fe-rich domains, which form during the transition from short- to long-range cation order.
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subjects Computer Simulation
Earth sciences
Earth, ocean, space
Exact sciences and technology
Geophysics: general, magnetic, electric and thermic methods and properties
Internal geophysics
Magnetics
Minerals - chemistry
Models, Chemical
title Origin of self-reversed thermoremanent magnetization
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