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Figure 11 | Earth, Planets and Space

Figure 11

From: Paleomagnetism and U-Pb geochronology of the late Cretaceous Chisulryoung Volcanic Formation, Korea: tectonic evolution of the Korean Peninsula

Figure 11

Variation of temporal clockwise rotations of the Korean Peninsula. Vertical rotations were calculated by comparing the observed and expected magnetic declination with respect to the three commonly used reference poles from China for Neogene (Zhao et al. 1994), Paleogene to Cretaceous (Huang et al. 2007), and Jurassic (Gilder and Courtillot 1997). Results from this study (red circles) indicate no significant rotation.

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