Many large-scale landslides have occurred along the active Pingding-Huama fault in
Zhouqu segment, Gansu, China. To better understand the failure mechanisms of these …

Old landslides in the Loess Plateau, Northwest China usually occurred over a relatively long
period, and their sizes are usually smaller compared to old landslides in the alpine valley …

In recent years, numerous ancient landslides initially triggered by historic earthquakes on
the eastern Tibetan Plateau have been reactivated by fault activity and heavy rainfall …

The investigation of reactivated landslides in the alpine-canyon areas suffers the difficult
accessibility of precipitous terrain. In particular, when reactivated landslides occur along the …

Ancient landslides tend to reactivate along pre‐existing slip zones that have reached a
residual state. On the eastern margin of the Tibetan Plateau, previous research has …

This study examines the Zhama ancient landslide, one of several large-scale ancient
landslides with complex formation mechanisms and significant reactivation trends found in …

The risk of reactivated ancient landslides in the Sichuan–Tibet transportation corridor in
China is significantly increasing, primarily driven by the intensification of engineering …

The reactivation of old landslides can be triggered by heavy destructive earthquakes, heavy
rainfall, and ongoing human activities, thereby resulting in the occurrence of secondary …

The identification of ancient landslides has become a challenging task due to the long-term
reconstruction and sediment cover, which obscure the original geomorphic characteristics of …

The Sichuan-Tibet transport corridor (STTC) is located at the eastern margin of the Tibetan
Plateau (TP), starting from Chengdu city of Sichuan province in the east and reaching Lasa …