Downcore variations of normalised relative paleointensity for CON01-603-2, VER98-1-1 and VER98-1-14.

Cite as:

Demory, Francois; Nowaczyk, Norbert; Witt, Annette; Oberhänsli, Hedi (2006): Downcore variations of normalised relative paleointensity for CON01-603-2, VER98-1-1 and VER98-1-14.. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1008

Status

I N R E V I E W : Demory, Francois; Nowaczyk, Norbert; Witt, Annette; Oberhänsli, Hedi (2006): Downcore variations of normalised relative paleointensity for CON01-603-2, VER98-1-1 and VER98-1-14.. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1008

Abstract

Selected intervals of down-core variations of normalised relative paleointensity, ChRM inclination and declination, and the reversal angle. (A) Core CON 01-603-2: numbers in the simplified lithological column indicate marine isotope stages (MIS), after Fig. 3. The paleomagnetic data show a geomagnetic excursion with a short, but full, reversal of the local field vector at the beginning of MIS 6. (B) Core VER 98-1-1: in this case, the excursion represented by a strong deviation of the reversal angle during a period of low intensity occurs in MIS 3 and corresponds to the Laschamp event. (C) Core VER 98-1-1: in this case, the excursion is also represented by a strong deviation of the reversal angle during a period of low intensity. Again this occurs in MIS 3 and corresponds to the Laschamp event.