Xu Tongchunup, Liu Xiumingup2, Yan Hongupp://dr=/. 1989: COMPARATIVE MEASUREMENTS OF MAGNETIC FABRIC BETWEEN KAPPA BRIDGES AND MINISEPS. Acta Seismologica Sinica, 11(3): 303-308.
Citation: Xu Tongchunup, Liu Xiumingup2, Yan Hongupp://dr=/. 1989: COMPARATIVE MEASUREMENTS OF MAGNETIC FABRIC BETWEEN KAPPA BRIDGES AND MINISEPS. Acta Seismologica Sinica, 11(3): 303-308.

COMPARATIVE MEASUREMENTS OF MAGNETIC FABRIC BETWEEN KAPPA BRIDGES AND MINISEPS

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  • Published Date: September 01, 2011
  • The Anisotropy of Magnetic Susceptibility (AMS) is a ubiquitous feature of rocks which reflects a tendency about the alignment of magnetic grains of minerals in it,i.e. magnetic fabric. In the last 30 years,the technique of magnetic fabric has been widely and efficiently applied to geology and geophysics,showing its prospects. Different principles are used for the development of instruments for AMS measurement. The consistency and reliability of the results obtained by different instruments should be checked and confirmed for a specimen through comparative measurements. The test was carried out by Kappa bridges (KLY-1,2) and Mi-niseps (Molspin Ltd.,U. K.) using cubic or cylindric specimens which are of different materials,i.e. loess,metamorphic rock,basalt or a compressed mixture of fault clay and SD magnetite. Consequently,(1) it is found that the repeatability of measurement by a Kappa bridge is often slightly better than that by a Minisep. (2) The calibration value for measuring the Kz depends on the susceptibility printed on the standard sample and the volumetric ratio of the standard specimen and to the specimen measured. And the calibration value for the spin measurement should be half the above-said calibration value for Kz measurement.
  • [1] Maher, B. A., 1996. Characterisation of soils by minera 1 magnetic measurements. Phys. Earth Piattct. Ints., 42. 76——92.

    [2] Walton, D., 1983. Viscous magnetisarion. Nature, 305, 61G——619.

    [3] Ising, E., 1942. On the magnetic properties of mrved clay. f'rkiu Tstror, Fysik, 29A(5), 1——37.

    [4] 许同春、刘秀铭、曹继秀,1987.岩石磁性组构的研究前景.国际地震动态,3: 1——6.

    [5] Hrouda, F., 1982. Wghetic anisotropy of rocks and its application in geology and geophysvcs. Geophys.Sura., S, 37——82.

    [6] 贺绍英、孙世伟,1985.用无定向磁力仪测量磁化率张量与剩余磁化强度矢量.物探与化探,9,281——288.

    [7] Hrouda, F,Stephenson, A., Woltar, L., 1983. On the standardization of measurements of the anisotropy of magnetic susceptibility. Phys. Earth Planet Ints., 32, 203——208.

    [8] Collinson, D. W., 1983. Methods in Rock Magnetism and Palacomagnetism——Techniques and Instrumen——tation Chapman & Hall, London. 503.

    [9] Scriba, H., Heller, F., 1978. Measurements of anisotropy of magnetic susceptibility using inductive magne——tometers. J. Geuphysics, 44, 341——352.

    [10] Fisher, R. A., 1953. Dispersion on a sphere, Proc. Roy. Soc., London, A217, 295——305.

    [1] Maher, B. A., 1996. Characterisation of soils by minera 1 magnetic measurements. Phys. Earth Piattct. Ints., 42. 76——92.

    [2] Walton, D., 1983. Viscous magnetisarion. Nature, 305, 61G——619.

    [3] Ising, E., 1942. On the magnetic properties of mrved clay. f'rkiu Tstror, Fysik, 29A(5), 1——37.

    [4] 许同春、刘秀铭、曹继秀,1987.岩石磁性组构的研究前景.国际地震动态,3: 1——6.

    [5] Hrouda, F., 1982. Wghetic anisotropy of rocks and its application in geology and geophysvcs. Geophys.Sura., S, 37——82.

    [6] 贺绍英、孙世伟,1985.用无定向磁力仪测量磁化率张量与剩余磁化强度矢量.物探与化探,9,281——288.

    [7] Hrouda, F,Stephenson, A., Woltar, L., 1983. On the standardization of measurements of the anisotropy of magnetic susceptibility. Phys. Earth Planet Ints., 32, 203——208.

    [8] Collinson, D. W., 1983. Methods in Rock Magnetism and Palacomagnetism——Techniques and Instrumen——tation Chapman & Hall, London. 503.

    [9] Scriba, H., Heller, F., 1978. Measurements of anisotropy of magnetic susceptibility using inductive magne——tometers. J. Geuphysics, 44, 341——352.

    [10] Fisher, R. A., 1953. Dispersion on a sphere, Proc. Roy. Soc., London, A217, 295——305.
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