Geomagnetic spikes on the core-mantle boundary

Rapid and spatially localized geomagnetic field variations around 1000 BC are hard to reconcile with expected field behaviour arising from the core dynamo. Here, the authors show that the intensity spike is consistent with an intense flux patch on the core-mantle boundary (8–22°) located under Saudi...

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Main Authors: Christopher Davies, Catherine Constable
Format: Article
Language:English
Published: Nature Publishing Group 2017-05-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/ncomms15593
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spelling doaj-7d04b49618e849c4bff093382a5fbd7a2021-05-11T07:44:17ZengNature Publishing GroupNature Communications2041-17232017-05-018111110.1038/ncomms15593Geomagnetic spikes on the core-mantle boundaryChristopher Davies0Catherine Constable1School of Earth & Environment, University of LeedsInstitute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California at San DiegoRapid and spatially localized geomagnetic field variations around 1000 BC are hard to reconcile with expected field behaviour arising from the core dynamo. Here, the authors show that the intensity spike is consistent with an intense flux patch on the core-mantle boundary (8–22°) located under Saudi Arabia.https://doi.org/10.1038/ncomms15593
collection DOAJ
language English
format Article
sources DOAJ
author Christopher Davies
Catherine Constable
spellingShingle Christopher Davies
Catherine Constable
Geomagnetic spikes on the core-mantle boundary
Nature Communications
author_facet Christopher Davies
Catherine Constable
author_sort Christopher Davies
title Geomagnetic spikes on the core-mantle boundary
title_short Geomagnetic spikes on the core-mantle boundary
title_full Geomagnetic spikes on the core-mantle boundary
title_fullStr Geomagnetic spikes on the core-mantle boundary
title_full_unstemmed Geomagnetic spikes on the core-mantle boundary
title_sort geomagnetic spikes on the core-mantle boundary
publisher Nature Publishing Group
series Nature Communications
issn 2041-1723
publishDate 2017-05-01
description Rapid and spatially localized geomagnetic field variations around 1000 BC are hard to reconcile with expected field behaviour arising from the core dynamo. Here, the authors show that the intensity spike is consistent with an intense flux patch on the core-mantle boundary (8–22°) located under Saudi Arabia.
url https://doi.org/10.1038/ncomms15593
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