Fig. 6From: A new method for the empirical conversion of logging data to clay mineral fraction in the Nankai accretionary prismData from the Kumano Basin sites. a Site C0002, b site C0009, and c a seismic profile around the Kumano Basin after Figure F116 of Expedition 319 Scientist (2010a). Symbols are the same as those in Figs. 2 and 5. Lsithological units colored by light blue represent the inner prism sediment below the Kumano Basin, which shows lower NGR log values than the standard sediments possibly due to poor hole conditionBack to article page