Nanoscale Imaging of High‐Field Magnetic Hysteresis in Meteoritic Metal Using X‐Ray Holography

Abstract Stable paleomagnetic information in meteoritic metal is carried by the “cloudy zone”: ~1–10 μm‐wide regions containing islands of ferromagnetic tetrataenite embedded in a paramagnetic antitaenite matrix. Due to their small size and high coercivity (theoretically up to ~2.2 T), the tetrataen...

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Main Authors: R. Blukis, B. Pfau, C. M. Günther, P. Hessing, S. Eisebitt, J. Einsle, R. J. Harrison
Format: Article
Language:English
Published: Wiley 2020-08-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2020GC009044
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author R. Blukis
B. Pfau
C. M. Günther
P. Hessing
S. Eisebitt
J. Einsle
R. J. Harrison
author_facet R. Blukis
B. Pfau
C. M. Günther
P. Hessing
S. Eisebitt
J. Einsle
R. J. Harrison
author_sort R. Blukis
collection DOAJ
description Abstract Stable paleomagnetic information in meteoritic metal is carried by the “cloudy zone”: ~1–10 μm‐wide regions containing islands of ferromagnetic tetrataenite embedded in a paramagnetic antitaenite matrix. Due to their small size and high coercivity (theoretically up to ~2.2 T), the tetrataenite islands carry very stable magnetic remanence. However, these characteristics also make it difficult to image their magnetic state with the necessary spatial resolution and applied magnetic field. Here, we describe the first application of X‐ray holography to image the magnetic structure of the cloudy zone of the Tazewell IIICD meteorite with spatial resolution down to ~40 nm and in applied magnetic fields up to ±1.1 T, sufficient to extract high‐field hysteresis data from individual islands. Images were acquired as a function of magnetic field applied both parallel and perpendicular to the surface of a ~100 nm‐thick slice of the cloudy zone. Broad distributions of coercivity are observed, including values that likely exceed the maximum applied field. Horizontal offsets in the hysteresis loops indicate an interaction field distribution with half width of ~100 mT between the islands in their room temperature single‐domain state, providing a good match to first‐order reversal curve diagrams. The results suggest that future models of remanence acquisition in the cloudy zone should take account of strong interactions in order to extract quantitative estimates of the paleofield.
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spelling doaj.art-0acad770255648f6afdd5acfec3affc02023-11-03T16:55:28ZengWileyGeochemistry, Geophysics, Geosystems1525-20272020-08-01218n/an/a10.1029/2020GC009044Nanoscale Imaging of High‐Field Magnetic Hysteresis in Meteoritic Metal Using X‐Ray HolographyR. Blukis0B. Pfau1C. M. Günther2P. Hessing3S. Eisebitt4J. Einsle5R. J. Harrison6GFZ German Centre for Geosciences Potsdam GermanyMax‐Born‐Institut Berlin GermanyCenter for Electron Microscopy (ZELMI) Technische Universität Berlin Berlin GermanyMax‐Born‐Institut Berlin GermanyMax‐Born‐Institut Berlin GermanySchool of Geographical and Earth Sciences University of Glasgow Glasgow UKDepartment of Earth Sciences University of Cambridge Cambridge UKAbstract Stable paleomagnetic information in meteoritic metal is carried by the “cloudy zone”: ~1–10 μm‐wide regions containing islands of ferromagnetic tetrataenite embedded in a paramagnetic antitaenite matrix. Due to their small size and high coercivity (theoretically up to ~2.2 T), the tetrataenite islands carry very stable magnetic remanence. However, these characteristics also make it difficult to image their magnetic state with the necessary spatial resolution and applied magnetic field. Here, we describe the first application of X‐ray holography to image the magnetic structure of the cloudy zone of the Tazewell IIICD meteorite with spatial resolution down to ~40 nm and in applied magnetic fields up to ±1.1 T, sufficient to extract high‐field hysteresis data from individual islands. Images were acquired as a function of magnetic field applied both parallel and perpendicular to the surface of a ~100 nm‐thick slice of the cloudy zone. Broad distributions of coercivity are observed, including values that likely exceed the maximum applied field. Horizontal offsets in the hysteresis loops indicate an interaction field distribution with half width of ~100 mT between the islands in their room temperature single‐domain state, providing a good match to first‐order reversal curve diagrams. The results suggest that future models of remanence acquisition in the cloudy zone should take account of strong interactions in order to extract quantitative estimates of the paleofield.https://doi.org/10.1029/2020GC009044X‐ray holographycloudy zoneTazewell meteorite
spellingShingle R. Blukis
B. Pfau
C. M. Günther
P. Hessing
S. Eisebitt
J. Einsle
R. J. Harrison
Nanoscale Imaging of High‐Field Magnetic Hysteresis in Meteoritic Metal Using X‐Ray Holography
Geochemistry, Geophysics, Geosystems
X‐ray holography
cloudy zone
Tazewell meteorite
title Nanoscale Imaging of High‐Field Magnetic Hysteresis in Meteoritic Metal Using X‐Ray Holography
title_full Nanoscale Imaging of High‐Field Magnetic Hysteresis in Meteoritic Metal Using X‐Ray Holography
title_fullStr Nanoscale Imaging of High‐Field Magnetic Hysteresis in Meteoritic Metal Using X‐Ray Holography
title_full_unstemmed Nanoscale Imaging of High‐Field Magnetic Hysteresis in Meteoritic Metal Using X‐Ray Holography
title_short Nanoscale Imaging of High‐Field Magnetic Hysteresis in Meteoritic Metal Using X‐Ray Holography
title_sort nanoscale imaging of high field magnetic hysteresis in meteoritic metal using x ray holography
topic X‐ray holography
cloudy zone
Tazewell meteorite
url https://doi.org/10.1029/2020GC009044
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