Intensity of the Earth's magnetic field: evidence for a Mid-Paleozoic dipole low-Reference-Cited by-同舟云学术

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Intensity of the Earth's magnetic field: evidence for a Mid-Paleozoic dipole low

Published:2020-08-25 Issue: Volume: Page:
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Author:

Hawkins Louise M. A.¹^ORCID,Grappone Joseph¹^ORCID,Sprain Courtney²^ORCID,Saengduean Patipan³,Sage Edward⁴,Thomas-Cunningham Sheikerra¹,Kugabalan Banusha⁵,Biggin Andrew¹^ORCID

Affiliation:

1. University of Liverpool

2. University of Floria

3. Colorado School of Mines

4. CGG Satellite Mapping

5. University of Glasgow

Funder

Natural Environment Research Council

University of Liverpool

Publisher

Wiley

Reference46 articles.

1. Bono, A Hadean to Paleoarchean geodynamo recorded by single zircon crystals;Tarduno J. A.;Science.,2015

2. Palaeomagnetic field intensity variations suggest Mesoproterozoic innercore nucleation;Biggin A. J.;Nature,2015

3. Cottrell, Young inner core inferred from Ediacaran ultra-low geomagnetic field intensity;Bono R. K.;Nat. Geosci.,2019

4. Gallet, A third superchron during the Early Paleozoic;Pavlov V.;Episodes,2005

5. Staudigel, Strength of the geomagnetic field in the Cretaceous Normal Superchron: New data from submarine basaltic glass of the Troodos Ophiolite. Geochemistry;Tauxe L.;Geophys. Geosystems,2004

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