Fig. 1.From: Paleointensity determination of Late Cretaceous basalts in northwest South Korea: implications for low and stable paleofield strength in the Late Cretaceous(a) Map of the Korean Peninsula showing the location of the study area. (b) Geologic map of the study area (modified from Kee et al., 2008). Solid circles represent the locations of sampling sites. Sites 1–4 and 11 are massive basalts and sites 5–10 are lava flows.Back to article page