Liquefaction within a bedding fault: Understanding the initiation and movement of the Daguangbao landslide triggered by the 2008 Wenchuan Earthquake (Ms= 8.0)
The Daguangbao landslide was the most catastrophic mass movement triggered by the
2008 Wenchuan earthquake with a magnitude scale of Ms. 8.0. The landslide, which was …
2008 Wenchuan earthquake with a magnitude scale of Ms. 8.0. The landslide, which was …
A rotary-shear low to high-velocity friction apparatus in Beijing to study rock friction at plate to seismic slip rates
This paper reviews 19 apparatuses having high-velocity capabilities, describes a rotary-
shear low to high-velocity friction apparatus installed at Institute of Geology, China …
shear low to high-velocity friction apparatus installed at Institute of Geology, China …
Investigation of influence of baffles on landslide debris mobility by 3D material point method
In mountainous terrain, landslide debris is a common occurrence around the world that can
potentially result in catastrophic consequences to downstream residents and facilities …
potentially result in catastrophic consequences to downstream residents and facilities …
Velocity‐dependent frictional weakening of large rock avalanche basal facies: Implications for rock avalanche hypermobility?
To characterize the hypermobility mechanism of rock avalanches, a series of rotary shear
tests at different shearing velocities (Veq) ranging from 0.07 m/s to 1.31 m/s and at a normal …
tests at different shearing velocities (Veq) ranging from 0.07 m/s to 1.31 m/s and at a normal …
Modelling large-scale landslide using a GPU-accelerated 3D MPM with an efficient terrain contact algorithm
The material point method (MPM) simulation of large-scale landslides can provide useful
information to response to landslide hazards in mountainous regions. However, the …
information to response to landslide hazards in mountainous regions. However, the …
Influence of grain contents on the dynamic strength of rock-like materials
MC Weng, HK Le, HH Li, TC Chen - Engineering Geology, 2024 - Elsevier
This study performed a series of uniaxial compressive tests and SHPB tests to investigate
the influence of grain content and loading rate on strength and failure mode of rock-like …
the influence of grain content and loading rate on strength and failure mode of rock-like …
Earthquake-driven acceleration of slow-moving landslides in the Colca valley, Peru, detected from Pléiades images
P Lacroix, E Berthier, ET Maquerhua - Remote Sensing of Environment, 2015 - Elsevier
Major earthquakes in mountainous areas often trigger rapid landslides. Some observations
also suggest that earthquakes can damage landslide prone areas or cause slow-moving …
also suggest that earthquakes can damage landslide prone areas or cause slow-moving …
Probabilistic analysis of a discrete element modelling of the runout behavior of the Jiweishan landslide
Landslide is one of the most destructive geohazards around the world. The destruction of a
landslide can be estimated from its deformation and runout behaviors, which might be …
landslide can be estimated from its deformation and runout behaviors, which might be …
Shear rate effect on the residual strength of saturated clayey and granular soils under low-to high-rate continuous shearing
H Miao, G Wang - Engineering Geology, 2022 - Elsevier
The residual strength of sliding basal soils plays a pivotal role not only in the movement of
bedding landslides controlled by clay-rich interlayers but also in remobilized granular …
bedding landslides controlled by clay-rich interlayers but also in remobilized granular …
Numerical modelling of the 2008 Wenchuan earthquake-triggered Daguangbao landslide using a velocity and displacement dependent friction law
Y Song, D Huang, D Cen - Engineering Geology, 2016 - Elsevier
Dynamic friction degradation of the sliding surface in large earthquake-triggered landslides
is widely assumed, especially for high-speed and long run-out landslides. But there are few …
is widely assumed, especially for high-speed and long run-out landslides. But there are few …