Holocene geocentric dipole tilt model constrained by sedimentary paleomagnetic data
Author:
Affiliation:
1. Department of Earth and Ecosystem Sciences; Lund University; Sölvegatan 12,; SE-223 62; Lund; Sweden
2. Division of Water Resources Engineering; Lund University; John Ericssons väg 1, V-huset,; SE-223 63; Lund; Sweden
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/gc/gc1008/2010GC003118/2010GC003118.pdf
Reference82 articles.
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2. Geomagnetic dipole tilt changes induced by core flow;Amit;Phys. Earth Planet. Inter.,2008
3. Compaction-induced inclination shallowing of the post-depositional remanent magnetization in a synthetic sediment;Anson;Geophys. J. R. Astron. Soc.,1987
4. A 10 000 yr geomagnetic secular variation record from three Australian maars;Barton;Geophys. J. Int.,1981
5. Holocene Earth's magnetic field variations recorded in marine sediments of the NW African continental margin;Bleil;Stud. Geophys. Geod.,2008
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