Fig. 2: Fault traces and typical fault landforms of the Jiali fault.
From: Spatial segmentation of Jiali Fault’s Holocene activity in the southeastern Tibetan Plateau
a Fault traces of the Jiali Fault from Yigong to Songzong town. Fault traces are obtained from seismotectonic maps of China and adjacent regions43, the geological structural database of the Qinghai-Tibet Plateau44 and the China Active Faults Database (CAFD)90. The map background shows the World Hillshade of the study region derived from the Esri in ArcGIS Online.; b–g typical fault landforms; b fault scarp near the Yigong barrier lake; c fault trench near Tongmai Bridge; d fault scarp near the Guxiang barrier lake; e fault trench near Bomi city; f linear landforms on the Podui River terrace; g linear fault valley near Galong La; h–j fault outcrops; h Shear zone and echelon fractures near Tongmai Bridge; i shear zone and ptygmatic fold near Tianmo Gully; j Slickolite and steps at the outcrop in eastern Bomi, revealing right-lateral strike-slip motion.
