Data Publications

High temperature measurement of the saturation magnetisation for VER98-1-14

hasData_Center_Short_Name
  • SDDB
hasDataset_Online_Resource
hasProject_Long_Name
  • Vereshchagin 98 Expedition
  • Vereshchagin Expedition 98
hasDataset_Release_Date
  • 2006-09-15
hasDataset_Title
  • High temperature measurement of the saturation magnetisation for VER98-1-14
hasEntry_ID
  • 10.1594/GFZ.SDDB.1027
hasKeyword
  • saturation magnetisation
  • temperature
hasReference
  • 10.1016/j.gloplacha.2004.11.010 http://dx.doi.org/10.1016/j.gloplacha.2004.11.010 Francois Demory, Hedi Oberhansli, Norbert R. Nowaczyk, Matthias Gottschalk, Richard Wirth and Rudolf Naumann, Detrital input and early diagenesis in sediments from Lake Baikal revealed by rock magnetism, Global and Planetary Change, Volume 46, Issues 1-4,
hasSummary
  • 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.
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