Fig. 1From: Investigating the utility of a high-temperature Thellier-style paleointensity experimental protocoltaken from Hodgson et al. (2018): (i) is the lower-temperature, higher-slope (overestimating) portion, (ii) is the higher-temperature, lower-slope (underestimating) portion, (iii) is the highest-temperature, most accurate portion that this current study aims to investigate furtherThe three zones of a non-single domain paleointensity experiment,Back to article page