Magnetization process of dirt-snow containing fine-grained magnetic minerals was investigated in order to understand the acquisition mechanism of natural remanent magnetization (NRM) by dirt-ice layers in Antarctica. Dirt-snow acquired NRM from the direction of geomagnetic field (GMF) direction at rooms -10°C and -20°C, and inclination becomes shallower than the GMF after 50 days. Probably the Antarctic dirt-ice has acquired NRM during the periods of accumulation of snow and magnetic grains and formation of the depth hoar. -from Authors
CITATION STYLE
Funaki, M., & Sakai, H. (1991). Acquistion of natural remanent magnetization for dirt-snow containing rock dust. Journal of Geomagnetism & Geoelectricity, 43(10), 803–811. https://doi.org/10.5636/jgg.43.803
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