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Global Geomagnetic Field Evolution From 900 to 700 ka Including the Matuyama‐Brunhes Reversal - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
Global Geomagnetic Field Evolution From 900 to 700 ka Including the Matuyama‐Brunhes Reversal - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
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Global Geomagnetic Field Evolution From 900 to 700 ka Including the Matuyama‐Brunhes Reversal - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
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Characteristics of the Matuyama‐Brunhes Magnetic Field Reversal Based on a Global Data Compilation - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
Global Geomagnetic Field Evolution From 900 to 700 ka Including the Matuyama‐Brunhes Reversal - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
Characteristics of the Matuyama‐Brunhes Magnetic Field Reversal Based on a Global Data Compilation - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
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Global Geomagnetic Field Evolution From 900 to 700 ka Including the Matuyama‐Brunhes Reversal - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
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Characteristics of the Matuyama‐Brunhes Magnetic Field Reversal Based on a Global Data Compilation - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
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Global Geomagnetic Field Evolution From 900 to 700 ka Including the Matuyama‐Brunhes Reversal - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
Characteristics of the Matuyama‐Brunhes Magnetic Field Reversal Based on a Global Data Compilation - Mahgoub - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library