| hasData_Center_Short_Name |
|
| hasDataset_Online_Resource |
|
| hasProject_Long_Name |
- Vereshchagin 98 Expedition
- Vereshchagin Expedition 98
|
| hasDataset_Release_Date |
|
| hasDataset_Title |
- High temperature measurement of the saturation magnetisation for VER98-1-1
|
| hasEntry_ID |
|
| 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.
|
| GCMD Sciencekeywords describing the dataset. Click on Keyword to find similar datasets | |
