Down-core variations of the inclination and declination of ChRM of all investigated cores.
Abstract Dashed lines mark some correlation levels of the cores from Lake Baikal with the dated δ18O record from ODP 677 (Shackleton et al., 1990), see also Fig. 3. Diagenetic features such as dissolution of magnetite and mineralization of greigite are marked according to Fig. 4. Laschamp and Icelan...
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ftgfzpotsdamdata:oai:doidb.wdc-terra.org:63 2023-05-15T16:49:25+02:00 Down-core variations of the inclination and declination of ChRM of all investigated cores. Demory, Francois Nowaczyk, Norbert Witt, Annette Oberhänsli, Hedi 51.5831 104.851 53.9632 108.9139 2006 6306 Datapoints text/tab-separated-values https://doi.org/10.1594/GFZ.SDDB.1011 eng eng Deutsches GeoForschungsZentrum GFZ doi:10.1016/j.gloplacha.2004.09.016 http://dx.doi.org/10.1594/GFZ.SDDB.1011 doi:10.1594/GFZ.SDDB.1011 Vereshchagin 98 Expedition Vereshchagin Long Cores Expedition 2001 R/V Vereshchagin declination (ChRM) inclination (ChRM) reversal angle (ChRM) stepwise demagnetisation DC-SQUID 755 SRM Dataset 2006 ftgfzpotsdamdata https://doi.org/10.1594/GFZ.SDDB.1011 https://doi.org/10.1016/j.gloplacha.2004.09.016 2022-03-10T11:14:19Z Abstract Dashed lines mark some correlation levels of the cores from Lake Baikal with the dated δ18O record from ODP 677 (Shackleton et al., 1990), see also Fig. 3. Diagenetic features such as dissolution of magnetite and mineralization of greigite are marked according to Fig. 4. Laschamp and Iceland Basin excursions are indicated as La. and Ic., respectively. Inclination and declination records could provide information on paleosecular variations (periodicity ≤105 years and directional variability <20°, according to Butler, 1992). In the present study, we did not interpret inclination and declination records in terms of paleosecular variations since slight sediment disturbances could produce slight deviations of ChRM declinations and inclinations. (see Fig.7) Dataset Iceland GFZ Data Services (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Shackleton |
institution |
Open Polar |
collection |
GFZ Data Services (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdamdata |
language |
English |
topic |
Vereshchagin 98 Expedition Vereshchagin Long Cores Expedition 2001 R/V Vereshchagin declination (ChRM) inclination (ChRM) reversal angle (ChRM) stepwise demagnetisation DC-SQUID 755 SRM |
spellingShingle |
Vereshchagin 98 Expedition Vereshchagin Long Cores Expedition 2001 R/V Vereshchagin declination (ChRM) inclination (ChRM) reversal angle (ChRM) stepwise demagnetisation DC-SQUID 755 SRM Demory, Francois Nowaczyk, Norbert Witt, Annette Oberhänsli, Hedi Down-core variations of the inclination and declination of ChRM of all investigated cores. |
topic_facet |
Vereshchagin 98 Expedition Vereshchagin Long Cores Expedition 2001 R/V Vereshchagin declination (ChRM) inclination (ChRM) reversal angle (ChRM) stepwise demagnetisation DC-SQUID 755 SRM |
description |
Abstract Dashed lines mark some correlation levels of the cores from Lake Baikal with the dated δ18O record from ODP 677 (Shackleton et al., 1990), see also Fig. 3. Diagenetic features such as dissolution of magnetite and mineralization of greigite are marked according to Fig. 4. Laschamp and Iceland Basin excursions are indicated as La. and Ic., respectively. Inclination and declination records could provide information on paleosecular variations (periodicity ≤105 years and directional variability <20°, according to Butler, 1992). In the present study, we did not interpret inclination and declination records in terms of paleosecular variations since slight sediment disturbances could produce slight deviations of ChRM declinations and inclinations. (see Fig.7) |
format |
Dataset |
author |
Demory, Francois Nowaczyk, Norbert Witt, Annette Oberhänsli, Hedi |
author_facet |
Demory, Francois Nowaczyk, Norbert Witt, Annette Oberhänsli, Hedi |
author_sort |
Demory, Francois |
title |
Down-core variations of the inclination and declination of ChRM of all investigated cores. |
title_short |
Down-core variations of the inclination and declination of ChRM of all investigated cores. |
title_full |
Down-core variations of the inclination and declination of ChRM of all investigated cores. |
title_fullStr |
Down-core variations of the inclination and declination of ChRM of all investigated cores. |
title_full_unstemmed |
Down-core variations of the inclination and declination of ChRM of all investigated cores. |
title_sort |
down-core variations of the inclination and declination of chrm of all investigated cores. |
publisher |
Deutsches GeoForschungsZentrum GFZ |
publishDate |
2006 |
url |
https://doi.org/10.1594/GFZ.SDDB.1011 |
op_coverage |
51.5831 104.851 53.9632 108.9139 |
geographic |
Shackleton |
geographic_facet |
Shackleton |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
doi:10.1016/j.gloplacha.2004.09.016 http://dx.doi.org/10.1594/GFZ.SDDB.1011 doi:10.1594/GFZ.SDDB.1011 |
op_doi |
https://doi.org/10.1594/GFZ.SDDB.1011 https://doi.org/10.1016/j.gloplacha.2004.09.016 |
_version_ |
1766039565197377536 |