A comparison of thermal and microwave palaeomagnetic techniques using lava containing laboratory induced remanence
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/151/1/157/1724140/151-1-157.pdf
Reference16 articles.
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2. Coe, R.S. , 1967. Paleo-Intensities of the Earth's magnetic field determined from Tertiary and Quaternary rocks, J. geophys. Res., 72, 3247-3263.
3. Coe, R.S. , Grommé, S. & Mankinen, E.A. , 1978. Geomagnetic paleointensities from radiocarbon-dated lava flows on Hawaii and the question of the Pacific nondipole low, J. geophys. Res., 83, 1740-1756.
4. Day, R. , Fuller, M.D. & Schmidt, V.A. , 1977. Hysteresis properties of titanomagnetites: grain size and composition dependence, Phys. Earth planet. Inter., 13, 260-266.
5. Hill, M.J. & Shaw, J. , 1999. Palaeointensity results for historic lavas from Mt. Etna using microwave demagnetization/remagnetization in a modified Thellier type experiment, Geophys. J. Int., 139, 583-590.
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