2026-06-18T03:24:03Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:1092026-06-10T10:05:21ZDOIDBDOIDB.SDDBfalse4DOIDB.SDDB
10.1594/GFZ.SDDB.1027
Demory, Francois
Oberhänsli, Hedi
Nowaczyk, Norbert
Gottschalk, Matthias
Wirth, Richard
Naumann, Rudolf
High temperature measurement of the saturation magnetisation for VER98-1-14
Deutsches GeoForschungsZentrum GFZ
2006
2006-09-15
Dataset
10.1016/j.gloplacha.2004.11.010
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.
107.969
53.523