In situ magnetic measurements on igneous rock bodies
- 47 Downloads
A simple method for an in situ measurement of susceptibility and low-field hysteresis on rock bodies like dykes and flows is described. Extensive use of this method indicates that in some dykes and flows, the nature of the magnetic grains varies rapidly across the bodies. Making use of such observations, it seems possible to select stable rock samples for palaeomagnetic work and also understand to some extent the origin of remanent magnetization in different types of rock bodies.
KeywordsSusceptibility hysteresis magnetic grains igneous rock bodies
Unable to display preview. Download preview PDF.
- Ade-Hall J M, Wilson R L and Smith P J 1965Earth Planet. Sci. Lett. 9 323Google Scholar
- Likhite S D and Radhakrishnamurty C 1965Bull. NGRI. 3 1Google Scholar
- Neel L 1970C. R. Acad. Sci. Paris 270 1125Google Scholar
- Radhakrishnamurty C and Deutsch E R 1974J. Geophys. 40 453Google Scholar
- Radhakrishnamurty C, Likhite S D, Raja P K S and Sahasrabudhe P W 1971Nature (London) Phys. Sci. 235 33Google Scholar
- Radhakrishnamurty C, Likhite S D, Deutsch E R and Murthy G S 1978 (in preparation)Google Scholar
- Radhakrishnamurty C and Sastry N P 1970Proc. Indian Acad. Sci. A72 94Google Scholar
- Soffel H 1975J. Geophys. 41 401Google Scholar