By S. Belomesnykh
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EMBLETON, B. J. J. 1981. Magnetic overprinting in southeastern Australia and the thermal history of its rifted margin. Journal of Geophysical Research, 86, 3998-4008. SPORER, H. 1984. On viscous remanent magnetization of synthetic multidomain magnetite. Geophysical Research Letters, 11, 209-212. TARLING, D. H. 1983 Palaeomagnetism. Chapman and Hall, London. TIVEY, M. & JOHNSON, H. P. 1984. The characterization of viscous remanent magnetization in large and small magnetite particles. Journal of Geophysical Research, 89B, 543-552.
Intermediate remanence component Youngest remanence component Fig. 12. The debris flow test. This provides slowly reoriented slump blocks that may record components of the geomagnetic field in different orientations within the sample, if the orientation changes rate at a similar pace to viscous remagnetization. This is superficially comparable with the conglomerate test of traditional palaeomagnetism (Tarling 1983), but an important difference exists. The conglomerate test represents one discrete reorientation of material that may, or may not, remagnetize after reorientation (Fig.
1969. An experimental evaluation of single domain theories. Reviews in Geophysics, 7, 709-757. --, NEWELL, A. J. & ENKIN, R. J. 1994. Transdomain thermoremanent magnetization. Journal of Geophysical Research, 99, 19741-19755. - - , 0ZDEM~R, O. & ENK~N, R. J. 1987. Multidomain and single-domain relations between susceptibility and coercive force, Physics of the Earth and Planetary Interiors, 49, 181-I 91. , & SCHMIDT, P. W. 1997a. Paleomagnetism and paleothermometry of the Sydney Basin: (2) Origin of anomalously high unblocking temperatures.