Palaeointensity determinations, using Coe's version of the Thellier method, for 7 flows on Hawaii are used to illustrate some of the problems in palaeointensity determinations by this method. It is shown that the linearity of NRM-TRM is not an adequate criterion for acceptance, but that it is very powerful when combined with the PTRM test. -from Authors
CITATION STYLE
Tanaka, H., & Kono, M. (1991). Preliminary results and reliability of palaeointensity studies on historical and 14C dated Hawaiian lavas. Journal of Geomagnetism & Geoelectricity, 43(5), 375–388. https://doi.org/10.5636/jgg.43.375
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