Normalised natural remanent magnetisation intensity during the last 240 000 years in piston cores from the central North Atlantic Ocean: geomagnetic field intensity or environmental signal?

Details Normalised natural remanent magnetisation intensity during the last 240 000 years in piston cores from the central North Atlantic Ocean: geomagnetic field intensity or environmental signal? Normalised natural remanent magnetisation intensity during the last 240 000 years in piston cores from the central North Atlantic Ocean: geomagnetic field intensity or environmental signal?

Jan 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995pepi...87..213w&link_type=ejournal

Physics of the Earth and Planetary Interiors, v. 87, p. 213-229

Physics

34

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