A study of gyroremanent magnetisation (GRM) and rotational remanent magnetisation (RRM) carried by greigite from lake sediments
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/151/2/469/5867993/151-2-469.pdf
Reference27 articles.
1. Dankers, P.H.M. & Zijderveld, J.D.A. , 1981. Alternating field demagnetisation of rocks, and the problem of gyromagnetic remanence, Earth planet. Sci. Lett., 53, 89-92.
2. Dekkers, M.J. & Schoonen, M.A.A. , 1996. Magnetic properties of hydrothermally synthesized greigite (F3S4); I, Rock magnetic parameters at room temperature, Geophys. J. Int., 126, 360-368.
3. Edwards, J. , 1982. Gyroremanent magnetisation produced by specimen rotation between successive alternating field treatments, Geophys. J. R. astr. Soc., 71, 199-214.
4. Hallam, D.F. & Maher, B.A. , 1994. A record of reversed polarity carried by the iron sulphide greigite in British early Pleistocene sediments, Earth planet. Sci. Lett., 121, 71-80.
5. Hoffmann, V. , 1992. Greigite : magnetic properties and first domain observations, Phys. Earth planet. Inter., 70, 288-301.
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