What we can learn about Mars from the magnetism of returned samples.

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Title: What we can learn about Mars from the magnetism of returned samples.
Authors: Weiss, Benjamin P.1 bpweiss@mit.edu, Mansbach, Elias N.1, Maurel, Clara2, Sprain, Courtney J.3, Swanson-Hysell, Nicholas L.4, Williams, Wyn5
Source: Proceedings of the National Academy of Sciences of the United States of America. 1/14/2025, Vol. 122 Issue 2, p1-10. 19p.
Subjects: Polar wandering, Mars (Planet), Magnetic measurements, Plate tectonics, Planetary atmospheres
Abstract: The Red Planet is a magnetic planet. The Martian crust contains strong magnetization from a core dynamo that likely was active during the Noachian period when the surface may have been habitable. The evolution of the dynamo may have played a central role in the evolution of the early atmosphere and the planet's transition to the current cold and dry state. However, the nature and history of the dynamo and crustal magnetization are poorly understood given the lack of well-preserved, oriented, ancient samples with geologic context available for laboratory study. Here, we describe how magnetic measurements of returned samples could transform our understanding of six key unknowns about Mars' planetary evolution and habitability. Such measurements could i) determine the history of the Martian dynamo field's intensity; ii) determine the history of the Martian dynamo field's direction; iii) test the hypothesis that Mars experienced plate tectonics or true polar wander; iv) constrain the thermal and aqueous alteration history of the samples; v) identify sources of Martian crustal magnetization and vi) characterize sedimentary and magmatic processes on Mars. We discuss how these goals can be achieved using future laboratory analyses of samples acquired by the Perseverance rover. [ABSTRACT FROM AUTHOR]
Copyright of Proceedings of the National Academy of Sciences of the United States of America is the property of National Academy of Sciences and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: What we can learn about Mars from the magnetism of returned samples.
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  Data: <searchLink fieldCode="AR" term="%22Weiss%2C+Benjamin+P%2E%22">Weiss, Benjamin P.</searchLink><relatesTo>1</relatesTo><i> bpweiss@mit.edu</i><br /><searchLink fieldCode="AR" term="%22Mansbach%2C+Elias+N%2E%22">Mansbach, Elias N.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Maurel%2C+Clara%22">Maurel, Clara</searchLink><relatesTo>2</relatesTo><br /><searchLink fieldCode="AR" term="%22Sprain%2C+Courtney+J%2E%22">Sprain, Courtney J.</searchLink><relatesTo>3</relatesTo><br /><searchLink fieldCode="AR" term="%22Swanson-Hysell%2C+Nicholas+L%2E%22">Swanson-Hysell, Nicholas L.</searchLink><relatesTo>4</relatesTo><br /><searchLink fieldCode="AR" term="%22Williams%2C+Wyn%22">Williams, Wyn</searchLink><relatesTo>5</relatesTo>
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  Data: <searchLink fieldCode="DE" term="%22Polar+wandering%22">Polar wandering</searchLink><br /><searchLink fieldCode="DE" term="%22Mars+%28Planet%29%22">Mars (Planet)</searchLink><br /><searchLink fieldCode="DE" term="%22Magnetic+measurements%22">Magnetic measurements</searchLink><br /><searchLink fieldCode="DE" term="%22Plate+tectonics%22">Plate tectonics</searchLink><br /><searchLink fieldCode="DE" term="%22Planetary+atmospheres%22">Planetary atmospheres</searchLink>
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  Data: The Red Planet is a magnetic planet. The Martian crust contains strong magnetization from a core dynamo that likely was active during the Noachian period when the surface may have been habitable. The evolution of the dynamo may have played a central role in the evolution of the early atmosphere and the planet's transition to the current cold and dry state. However, the nature and history of the dynamo and crustal magnetization are poorly understood given the lack of well-preserved, oriented, ancient samples with geologic context available for laboratory study. Here, we describe how magnetic measurements of returned samples could transform our understanding of six key unknowns about Mars' planetary evolution and habitability. Such measurements could i) determine the history of the Martian dynamo field's intensity; ii) determine the history of the Martian dynamo field's direction; iii) test the hypothesis that Mars experienced plate tectonics or true polar wander; iv) constrain the thermal and aqueous alteration history of the samples; v) identify sources of Martian crustal magnetization and vi) characterize sedimentary and magmatic processes on Mars. We discuss how these goals can be achieved using future laboratory analyses of samples acquired by the Perseverance rover. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
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  Data: <i>Copyright of Proceedings of the National Academy of Sciences of the United States of America is the property of National Academy of Sciences and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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        Value: 10.1073/pnas.2404259121
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        Text: English
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        PageCount: 19
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        Type: general
      – SubjectFull: Mars (Planet)
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      – SubjectFull: Magnetic measurements
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      – SubjectFull: Plate tectonics
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      – SubjectFull: Planetary atmospheres
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      – TitleFull: What we can learn about Mars from the magnetism of returned samples.
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              Text: 1/14/2025
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