Down-core variations of anhysteretic remanent magnetisation and simplified lithological description of the investigated cores.

DOI

Conceptual intercorrelation between ARM and simplified lithology and correlation to the δ18O record from ODP Site 677 (Shackleton et al., 1990), assuming that clay-rich layers with high magnetic concentration represent glacial periods, and that diatomaceous layers with low magnetic concentration represent interglacial periods. Numbers in the δ18O record represent marine isotope stages (MIS).

Identifier
DOI https://doi.org/10.1594/GFZ.SDDB.1004
Related Identifier https://doi.org/10.1016/j.gloplacha.2004.09.016
Related Identifier https://doi.org/10.1016/S0040-1951(03)00197-5
Metadata Access http://doidb.wdc-terra.org/oaip/oai?verb=GetRecord&metadataPrefix=oai_datacite&identifier=oai:doidb.wdc-terra.org:205
Provenance
Creator Demory, Francois; Nowaczyk, Norbert; Witt, Annette; Oberhänsli, Hedi
Publisher Deutsches GeoForschungsZentrum GFZ
Publication Year 2006
OpenAccess true
Contact www.icdp-online.org/contact
Representation
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 2464 Datapoints
Discipline Scientific drilling
Spatial Coverage (104.851W, 51.583S, 108.914E, 53.963N)