Self‐Reversed Magnetization in Sediments Caused by Greigite Alteration

Abstract Multipolarity remanence in greigite‐bearing sediments has long been recognized, but the cause of this anomalous remanence behavior is not well understood. Here, we use electron microscopic and magnetic analyses to investigate the origin of such multipolarity in Miocene greigite‐bearing sedi...

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Bibliographic Details
Main Authors: Liao Chang, Zhaowen Pei, Pengfei Xue, Shishun Wang, Zhaoping Wang, Wout Krijgsman, Mark J. Dekkers
Format: Article
Language:English
Published: Wiley 2023-06-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2023GL103885