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Fig. 6 | Earth, Planets and Space

Fig. 6

From: Archeointensity estimates of a tenth-century kiln: first application of the Tsunakawa–Shaw paleointensity method to archeological relics

Fig. 6

a, b Typical results of the Tsunakawa–Shaw method. All the samples show similar graph patterned in common (NRM-TRM1 and ARM0-ARM1 ratios show extremely high linearity). The 3 diagrams on the left side show results from the first laboratory heating. The 3 diagrams on the right side show results from the second laboratory heating

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