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

<div>Cross section A-A′. See Figure <a href="../fig4/">4</a> for its location. S<sub>2</sub>s: Silurian Shimenkan formation, P<sub>1</sub>: lower Permian strata, P<sub>2</sub><i>β</i>: Permian Emeishan basalt, P<sub>2</sub>1: Permian Leping formation, T<sub>1</sub>f + t: Triassic Feixianguan and Tongjiezi formations, and T<sub>1</sub>j: Triassic Jialingjiang formation.</div>

Advances in Civil Engineering

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Figure 6

Figure 6: 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 | The Activity of the Yaziba Fault on the Lower Reaches of the Jinsha River, Southwestern China: Indirect Evidence from Paleo Earthquakes and Ancient Landslides 