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Fig. 5. | Earth, Planets and Space

Fig. 5.

From: Paleointensity determination of Late Cretaceous basalts in northwest South Korea: implications for low and stable paleofield strength in the Late Cretaceous

Fig. 5.

(a–c) Representative results of the thermal demagnetization of 3-axis isothermal remanent magnetization. Squares, circles, and triangles represent low- (<0.12 T), intermediate- (= 0.12–0.6 T), and high-coercivity (= 0.6–2.5 T) components, respectively. (d–f) Temperature dependence of the magnetic susceptibility (k-T) curves for selected samples.

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