Abstract

AbstractStable 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.

Highlights

  • The results presented represent the average of 100 separate simulations, each generated with a random placement of particles and easy axes, and a new random assignment of coercivities from the distribution observed in X‐ray holography

  • Simulated images of hypothetical cloudy zone structures demonstrated that this effect was primarily caused by overlapping islands and a large matrix contribution to the signal, the presence of some 2‐D islands cannot be ruled out

  • FORCulator simulations using the experimentally measured coercivity distribution from the out‐of‐plane data set produced similar offset distributions to those observed using X‐ray holography, the distribution was narrower and more similar to that observed in the in‐plane data set

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Summary

Introduction

Magnetic Fields in the Early Solar System. A longer‐lived source of magnetic fields in the early solar system comes from differentiated planetesimals, which are thought to have generated BLUKIS ET AL. Evidence of both nebular and planetesimal fields is obtained from the meteorite record (Bryson et al, 2015; Fu et al, 2012, 2014). The ability to make quantitative paleomagnetic measurements of past magnetic fields from meteorites is an important tool for constraining astrophysical models of star system formation and the thermal, chemical, and physical properties of planetesimals

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