| hasData_Center_Short_Name |
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| hasDataset_Online_Resource |
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| hasProject_Long_Name |
- Vereshchagin 98 Expedition
- Vereshchagin Expedition 98
- Vereshchagin Long Cores Expedition 2001
- High-resolution CONTINENTal paleoclimate record in Lake Baikal
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| hasDataset_Release_Date |
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| hasDataset_Title |
- Downcore variations of normalised relative paleointensity for CON01-603-2, VER98-1-1 and VER98-1-14.
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| hasEntry_ID |
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| hasKeyword |
- normalised relative palaeointensity
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| hasReference |
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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,
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| hasSummary |
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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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| GCMD Sciencekeywords describing the dataset. Click on Keyword to find similar datasets | |
