Fig. 3From: Timing of clockwise rotation of Southwest Japan: constraints from new middle Miocene paleomagnetic resultsMap of the Shuku locality, showing locations of paleomagnetic sampling sites in the eastern and western stratigraphic sections of the Oidawara Formation. Arrows on both sections indicate the younging direction. The red line is the surface trace of the fine felsic tuff bed in the middle of the Oidawara Formation; gray dashed lines are topographic contoursBack to article page