Fig. 4: Outcrop of Holocene sediment cut by the Jiali Fault.
From: Spatial segmentation of Jiali Fault’s Holocene activity in the southeastern Tibetan Plateau
a Panorama photograph of the outcrop; the white dashed box indicates the position of subsequent photographs c–e. b Details of the position of fault deformation. c Details of the deformation and fracturing of the silty sand layer and the fault distance. d Details of unit P. Small gravel clasts have low roundness, and large pebbles have high roundness. e Details of unit A, which is not crossed by a fault.
