A long-lived planetesimal dynamo powered by core crystallization

The existence of numerous iron meteorite groups indicates that some planetesimals underwent melting that led to metal‐silicate segregation, sometimes producing metallic cores. Meteorite paleomagnetic records suggest that crystallization of these cores generated dynamo magnetic fields. Here we descri...

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Main Authors: Maurel, C, Bryson, JFJ, Shah, J, Chopdekar, RV, Elkins-Tanton, LT, Raymond, CA, Weiss, BP
Format: Journal article
Language:English
Published: Wiley 2021
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author Maurel, C
Bryson, JFJ
Shah, J
Chopdekar, RV
Elkins-Tanton, LT
Raymond, CA
Weiss, BP
author_facet Maurel, C
Bryson, JFJ
Shah, J
Chopdekar, RV
Elkins-Tanton, LT
Raymond, CA
Weiss, BP
author_sort Maurel, C
collection OXFORD
description The existence of numerous iron meteorite groups indicates that some planetesimals underwent melting that led to metal‐silicate segregation, sometimes producing metallic cores. Meteorite paleomagnetic records suggest that crystallization of these cores generated dynamo magnetic fields. Here we describe the magnetic history of the partially differentiated IIE iron meteorite parent body. This is the first planetesimal for which we have a time‐resolved paleomagnetic record constrained by 40Ar/39Ar chronometry spanning several tens of million years (Ma). We find that the core of the IIE parent body generated a dynamo, likely powered by core crystallization, starting before 78 ± 13 Ma after solar system formation and lasting at least 80 Ma. Such extended core crystallization suggests that the core composed a substantial fraction of the body ( >~ 13%–19% core‐to‐body radius ratio depending on the body’s radius), indicating efficient core formation within some partially differentiated planetesimals.
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spelling oxford-uuid:27f9a88e-2063-4914-a69e-8be0377b42372022-03-26T12:10:14ZA long-lived planetesimal dynamo powered by core crystallizationJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:27f9a88e-2063-4914-a69e-8be0377b4237EnglishSymplectic ElementsWiley2021Maurel, CBryson, JFJShah, JChopdekar, RVElkins-Tanton, LTRaymond, CAWeiss, BPThe existence of numerous iron meteorite groups indicates that some planetesimals underwent melting that led to metal‐silicate segregation, sometimes producing metallic cores. Meteorite paleomagnetic records suggest that crystallization of these cores generated dynamo magnetic fields. Here we describe the magnetic history of the partially differentiated IIE iron meteorite parent body. This is the first planetesimal for which we have a time‐resolved paleomagnetic record constrained by 40Ar/39Ar chronometry spanning several tens of million years (Ma). We find that the core of the IIE parent body generated a dynamo, likely powered by core crystallization, starting before 78 ± 13 Ma after solar system formation and lasting at least 80 Ma. Such extended core crystallization suggests that the core composed a substantial fraction of the body ( >~ 13%–19% core‐to‐body radius ratio depending on the body’s radius), indicating efficient core formation within some partially differentiated planetesimals.
spellingShingle Maurel, C
Bryson, JFJ
Shah, J
Chopdekar, RV
Elkins-Tanton, LT
Raymond, CA
Weiss, BP
A long-lived planetesimal dynamo powered by core crystallization
title A long-lived planetesimal dynamo powered by core crystallization
title_full A long-lived planetesimal dynamo powered by core crystallization
title_fullStr A long-lived planetesimal dynamo powered by core crystallization
title_full_unstemmed A long-lived planetesimal dynamo powered by core crystallization
title_short A long-lived planetesimal dynamo powered by core crystallization
title_sort long lived planetesimal dynamo powered by core crystallization
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