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Detailed Reference Information |
Dekkers, M.J., Mattéi, J.-L., Fillion, G. and Rochette, P. (1989). Grain-size dependence of the magnetic behavior of pyrrhotite during its low-temperature transition at 34 K. Geophysical Research Letters 16: doi: 10.1029/89GL01286. issn: 0094-8276. |
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The grain-size dependent behavior of pyrrhotite during a magnetic LT-transition at 34 K is suitable for granulometric purposes. Cycling down to liquid Helium temperature suppresses soft MD Jrs more than hard SD Jrs, so that it may be effective in removing soft secondary NRM components. The domain structure of large pyrrhotite grains changes from MD at room temperature to SD or PSD below the LT-transition. ¿ American Geophysical Union 1989 |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Geomagnetism and Paleomagnetism, Rock and mineral magnetism |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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