Data Publications

Down-core variations of the reversal angle of the ChRM for VER98-1-1 and VER98-1-14

hasData_Center_Short_Name
  • SDDB
hasDataset_Online_Resource
hasProject_Long_Name
  • Vereshchagin 98 Expedition
  • Vereshchagin Expedition 98
hasDataset_Release_Date
  • 2006-09-13
hasDataset_Title
  • Down-core variations of the reversal angle of the ChRM for VER98-1-1 and VER98-1-14
hasEntry_ID
  • 10.1594/GFZ.SDDB.1010
hasKeyword
  • reversal angle (ChRM)
hasReference
  • 10.1016/j.gloplacha.2004.09.016 http://dx.doi.org/10.1016/j.gloplacha.2004.09.016 Francois Demory, Norbert R. Nowaczyk, Annette Witt and Hedi Oberhansli, High-resolution magnetostratigraphy of late quaternary sediments from Lake Baikal, Siberia: timing of intracontinental paleoclimatic responses, Global and Planetary Change, Volume 46,
hasSummary
  • 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.
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