High temperature measurement of the saturation magnetisation for VER98-1-14
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http://dataservices.gfz.de/SDDB/showshort.php?id=escidoc%3A76071
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资源简介：
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.
提供机构：
Deutsches GeoForschungsZentrum GFZ
创建时间：
2011-12-13
