Dataset
Data Publication
High temperature measurement of the saturation magnetisation for VER98-1-1
Demory, Francois | Oberhänsli, Hedi | Nowaczyk, Norbert | Gottschalk, Matthias | Wirth, Richard | Naumann, Rudolf
Deutsches GeoForschungsZentrum GFZ
(2006)
Descriptions
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.
Keywords
MSL enriched keywords
Measured property
magnetic hysteresis curves
hysteresis parameters
saturation magnetisation
minerals
sulfide minerals
greigite
oxide mineral
magnetite
Metadata
MSL enriched sub domains
paleomagnetism
Resource Type
Source
Source publisher
| Deutsches GeoForschungsZentrum GFZ |
Creators
| Demory, Francois |
| Personal |
| Oberhänsli, Hedi |
| Personal |
| Nowaczyk, Norbert |
| Personal |
| Gottschalk, Matthias |
| Personal |
| Wirth, Richard |
| Personal |
| Naumann, Rudolf |
| Personal |
Citation
Demory, F., Oberhänsli, H., Nowaczyk, N., Gottschalk, M., Wirth, R., & Naumann, R. (2006). High temperature measurement of the saturation magnetisation for VER98-1-1 [Dataset]. Deutsches GeoForschungsZentrum GFZ. https://doi.org/10.1594/GFZ.SDDB.1028
Dates
| Issued | 2006-09-15 |
Language
en