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Detailed Reference Information |
Borradaile, G.J. and Stupavsky, M. (1995). Anisotropy of magnetic susceptibility: Measurement schemes. Geophysical Research Letters 22: doi: 10.1029/95GL01910. issn: 0094-8276. |
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The precision of AMS determination is enhanced by measuring susceptibility in directions with a uniform orientation distribution that include the four body diagonals. Some standard 10.5 cm3 samples with mean susceptibility <100&mgr;SI possess too few ''magnetic'' grains for reliable petrofabric interpretation whatever the measurement strategy. We should only interpret their AMS if they pass fabric homogeneity tests. ¿ American Geophysical Union 1995 The precision of AMS determination is enhanced by measuring susceptibility in directions with a uniform orientation distribution that include the four body diagonals. Some standard 10.5 cm3 samples with mean susceptibility <100&mgr;SI possess too few ''magnetic'' grains for reliable petrofabric interpretation whatever the measurement strategy. We should only interpret their AMS if they pass fabric homogeneity tests. ¿ American Geophysical Union 1995 |
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Abstract |
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Keywords
Geomagnetism and Paleomagnetism, Magnetic fabrics and anisotropy |
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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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