Dataset
Data Publication
Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis
Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi
Deutsches GeoForschungsZentrum GFZ
(2006)
Descriptions
Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis (magnetite dissolution and/or greigite formation) and correlation to the relative paleointensity record from ODP Site 984 (Channell, 1999). In addition to AMS 14C dating and the geomagnetic excursions, the age model was completed and refined by tuning the relative paleointensity records to the equivalent record from ODP Site 984 (Channell, 1999; Fig. 8). The relative paleointensity variations in Lake Baikal and ODP Site 984 are well correlated. This confirms the global geomagnetic field origin of the relative paleointensity variations documented in the present study. In addition, it shows that local sedimentary variations have no effect on the paleomagnetic records.
Keywords
Originally assigned keywords
MSL enriched keywords
Metadata
MSL enriched sub domains
Resource Type
Source publisher
| Deutsches GeoForschungsZentrum GFZ |
DOI
| 10.1594/gfz.sddb.1012 |
Creators
| Demory, Francois |
| Personal |
| Nowaczyk, Norbert |
| Personal |
| Witt, Annette |
| Personal |
| Oberhänsli, Hedi |
| Personal |
Citation
Demory, F., Nowaczyk, N., Witt, A., & Oberhänsli, H. (2006). Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis [Data set]. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1012
Dates
| Issued | 2006-09-13 |
Language
en
Locations
- no geo-locations found -