Determining Individual Particle Magnetizations in Assemblages of Micrograins

Journal Article (2018)
Author(s)

L.V. de Groot (Universiteit Utrecht)

Karl Fabian (Geological Survey of Norway)

Annemarieke Béguin (Universiteit Utrecht)

Pim Reith (University of Twente)

A Barnhoorn (TU Delft - Applied Geophysics and Petrophysics)

Hans Hilgenkamp (University of Twente)

Research Group
Applied Geophysics and Petrophysics
Copyright
© 2018 L.V. de Groot, Karl Fabian, Annemarieke Béguin, Pim Reith, A. Barnhoorn, Hans Hilgenkamp
DOI related publication
https://doi.org/10.1002/2017GL076634
More Info
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Publication Year
2018
Language
English
Copyright
© 2018 L.V. de Groot, Karl Fabian, Annemarieke Béguin, Pim Reith, A. Barnhoorn, Hans Hilgenkamp
Research Group
Applied Geophysics and Petrophysics
Issue number
7
Volume number
45
Pages (from-to)
2995-3000
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Abstract

Obtaining reliable information from even the most challenging paleomagnetic recorders, such as the oldest igneous rocks and meteorites, is paramount to open new windows into Earth's history. Currently, such information is acquired by simultaneously sensing millions of particles in small samples or single crystals using superconducting quantum interference device magnetometers. The obtained rock-magnetic signal is a statistical ensemble of grains potentially differing in reliability as paleomagnetic recorder due to variations in physical dimensions, chemistry, and magnetic behavior. Here we go beyond bulk magnetic measurements and combine computed tomography and scanning magnetometry to uniquely invert for the magnetic moments of individual grains. This enables us to select and consider contributions of subsets of grains as a function of particle-specific selection criteria and avoid contributions that arise from particles that are altered or contain unreliable magnetic carriers. This new, nondestructive, method unlocks information from complex paleomagnetic recorders that until now goes obscured.