Figure 2From: Characterizing magnetic mineral assemblages of surface sediments from major Asian dust sources and implications for the Chinese loess magnetismLow-temperature thermal demagnetization of SIRM curves for the non-CLP (a-f) and CLP sources (g-j). The dashed vertical lines indicate the Verwey transition temperature at 120 K for stoichiometric magnetite. The variable magnitude of the Verwey transition indicates that magnetite in the samples has undergone variable degrees of low-temperature oxidization.Back to article page