High temperature measurement of the saturation magnetisation for VER98-1-1

DOI

It shows a loss of a part of the signal at temperatures between 350 and 400 °C, typical disintegration temperatures for greigite. The remaining signal disappears above a temperature of 590 °C, typical for magnetite.

Identifier
DOI https://doi.org/10.1594/GFZ.SDDB.1028
Related Identifier https://doi.org/10.1016/j.gloplacha.2004.11.010
Metadata Access http://doidb.wdc-terra.org/oaip/oai?verb=GetRecord&metadataPrefix=oai_datacite&identifier=oai:doidb.wdc-terra.org:106
Provenance
Creator Demory, Francois; Oberhänsli, Hedi; Nowaczyk, Norbert; Gottschalk, Matthias; Wirth, Richard; Naumann, Rudolf
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 516 Datapoints
Discipline Scientific drilling
Spatial Coverage (107.923 LON, 53.393 LAT)