2026-05-14T07:48:39Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:1082016-11-25T15:10:28ZDOIDBDOIDB.SDDBfalse3DOIDB.SDDB
10.1594/GFZ.SDDB.1010
Demory, Francois
Nowaczyk, Norbert
Witt, Annette
Oberhänsli, Hedi
Down-core variations of the reversal angle of the ChRM for VER98-1-1 and VER98-1-14
Deutsches GeoForschungsZentrum GFZ
2006
Vereshchagin 98 Expedition
R/V Vereshchagin
reversal angle (ChRM)
stepwise demagnetisation
DC-SQUID 755 SRM
2006-09-13
eng
Dataset
10.1016/j.gloplacha.2004.09.016
156 Datapoints
text/tab-separated-values
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.
53.3933 107.9227 53.523 107.9694