Fig. 2From: Depth profile of frictional properties in the inner Nankai accretionary prism using cuttings from IODP Site C0002Pressure, clay mineral content, and unit classification profiles for Site C0002 (after Tobin et al. 2015, 2020; Underwood 2017a, b; Kitajima et al. 2020). The lithospheric pressure is calculated from the overburden stress, which is derived from the rock density, and the hydrostatic pore pressure is calculated using a fluid density of 1.024Â g/cm3Back to article page