Fig. 5.From: Paleointensity determination of Late Cretaceous basalts in northwest South Korea: implications for low and stable paleofield strength in the Late Cretaceous(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.Back to article page