2026-05-14T08:12:03Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:712016-11-25T15:10:36ZDOIDBDOIDB.SDDBfalse3DOIDB.SDDB
10.1594/GFZ.SDDB.1017
Demory, Francois
Nowaczyk, Norbert
Witt, Annette
Oberhänsli, Hedi
Paleointensity versus age of all the sedimentary sequences of the present study
Deutsches GeoForschungsZentrum GFZ
2006
Vereshchagin 98 Expedition
Vereshchagin Long Cores Expedition 2001
R/V Vereshchagin
age (calendar years)
calculation
correlation
normalised relative palaeointensity
2006-09-15
eng
Dataset
10.1016/j.gloplacha.2004.09.016
3656 Datapoints
text/tab-separated-values
Paleointensity versus age of all the sedimentary sequences of the present study, of the synthetic curve resulting from its compilation from other curves, and of the reference curve from ODP Site 984 (Channell, 1999). For the compilation, data have been averaged using a sliding window of 2 ka (the variance is marked by the grey shadow). Dashed lines show some of the correlations. The grey lines show the location of the low paleointensities related to geomagnetic excursions. Note that the lowest paleointensities in the time span of Blake are at c. 129 ka. (see Fig.11)
51.5831 104.851 53.9632 108.9139