Advances in Civil Engineering / 2019 / Article / Fig 6

Research Article

The Activity of the Yaziba Fault on the Lower Reaches of the Jinsha River, Southwestern China: Indirect Evidence from Paleo Earthquakes and Ancient Landslides

Figure 6

Cross section A-A′. See Figure 4 for its location. S2s: Silurian Shimenkan formation, P1: lower Permian strata, P2β: Permian Emeishan basalt, P21: Permian Leping formation, T1f + t: Triassic Feixianguan and Tongjiezi formations, and T1j: Triassic Jialingjiang formation.

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