Behaviour of the geomagnetic field during the Matuyama–Brunhes polarity transition
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Reference45 articles.
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3. Exploring the influence of a time-varying non-dipole field on magnetic records for field reversals and excursions;Brown,2005
4. Geomagnetic palaeointensities and astrochronological ages for the Matuyama–Brunhes boundary and the boundaries of the Jaramillo Subchron: palaeomagnetic and oxygen isotope records from ODP site 983;Channell;Phil. Trans. R. Soc. Lond. A,2000
5. The Matuyama–Brunhes boundary interval (500–900ka) in North Atlantic drift sediments;Channell;Geophys. J. Int.,2004
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1. Robustness of characteristics of the Matuyama-Brunhes geomagnetic field reversal found in global models;Frontiers in Earth Science;2024-08-15
2. Global Geomagnetic Field Evolution From 900 to 700 ka Including the Matuyama‐Brunhes Reversal;Journal of Geophysical Research: Solid Earth;2023-06
3. Characteristics of the Matuyama‐Brunhes Magnetic Field Reversal Based on a Global Data Compilation;Journal of Geophysical Research: Solid Earth;2023-02
4. Fast Directional Changes during Geomagnetic Transitions: Global Reversals or Local Fluctuations?;Geosciences;2021-07-28
5. A paleomagnetic record of the early Matuyama chron including the Réunion subchron and the onset Olduvai boundary: High-resolution magnetostratigraphy and insights from transitional geomagnetic fields;Progress in Earth and Planetary Science;2020-08-08
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