Results 21 to 30 of about 592,574 (222)

Predicting seismic landslide hazard in the Batang fault zone of the Qinghai-Tibet Plateau

open access: yesShuiwen dizhi gongcheng dizhi, 2021
The Batang fault on the eastern Qinghai-Tibet Plateau has strong activity since the Holocene, where the geomorphology and geological structure is complex, and the historical earthquakes occurred frequently, which induced abundant landslides. For the long-
Zhihua YANG   +4 more
doaj   +1 more source

Effects of finite source rupture on landslide triggering: the 2016 Mw 7.1 Kumamoto earthquake [PDF]

open access: yesSolid Earth, 2019
The propagation of a seismic rupture on a fault introduces spatial variations in the seismic wave field surrounding the fault. This directivity effect results in larger shaking amplitudes in the rupture propagation direction.
S. von Specht   +10 more
doaj   +1 more source

Study on the Dynamic Response of Landslide Subjected to Earthquake by the Improved DDA Method

open access: yesModelling and Simulation in Engineering, 2021
Majiagou landslide, a major ancient landslide in Three Gorges Reservoir region, is located in the high earthquake area of southwest China. The 2013 Badong earthquake caused an obvious deformation of landslide monitored by the sliding inclinometer.
Xiu-Li Zhang   +3 more
doaj   +1 more source

Monitoring and Assessment for the Susceptibility of Landslide Changes After the 2017 Ms 7.0 Jiuzhaigou Earthquake Using the Remote Sensing Technology

open access: yesFrontiers in Earth Science, 2021
Monitoring the change of post-seismic landslides could provide valuable information for geological disaster treatment. The 2017 Jiuzhaigou Ms 7.0 earthquake has triggered a large number of landslides in the Jiuzhaigou United Nations Educational ...
Xinyi Guo   +14 more
doaj   +1 more source

Rapid assessment of seismic landslide zones [PDF]

open access: yesJournal of Modern Transportation, 2015
In the feasibility stage of the transport route selection, large-scale geological investigations are advised before the route is determined. Therefore, rapid assessment of seismic landslide zones can be completed by the second development of the ArcGIS program.
Haiqiang Guo, Lingkan Yao, Shaowei Sun
openaire   +1 more source

Landslide Susceptibility Mapping and Interpretation in the Upper Minjiang River Basin

open access: yesRemote Sensing, 2023
To enable the accurate assessment of landslide susceptibility in the upper reaches of the Minjiang River Basin, this research intends to spatially compare landslide susceptibility maps obtained from unclassified landslides directly and the spatial ...
Xin Wang, Shibiao Bai
doaj   +1 more source

Towards Automatic Landslide-Quake Identification Using a Random Forest Classifier

open access: yesApplied Sciences, 2020
Landslide-generated seismic waves (landslide-quakes), exhibiting distinctive waveforms and frequency characteristics, can be recorded by nearby seismometers.
Guan-Wei Lin   +6 more
doaj   +1 more source

Distribution of large- and medium-scale loess landslides induced by the Haiyuan Earthquake in 1920 based on field investigation and interpretation of satellite images

open access: yesOpen Geosciences, 2022
Studying the distribution law and influencing factors of coseismic landslides has important scientific significance and engineering value for understanding the mechanism of seismic landslides and predicting the occurrence of seismic landslides.
Chang Chaoyu   +4 more
doaj   +1 more source

Front Matter

open access: yesGeophysical Monograph Series, Page i-xiv., 2021

Exploring the links between Large Igneous Provinces and dramatic environmental impact

An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
wiley  

+1 more source

Dynamics of the Askja caldera July 2014 landslide, Iceland, from seismic signal analysis: precursor, motion and aftermath [PDF]

open access: yesEarth Surface Dynamics, 2018
Landslide hazard motivates the need for a deeper understanding of the events that occur before, during, and after catastrophic slope failures. Due to the destructive nature of such events, in situ observation is often difficult or impossible. Here, we
A. Schöpa   +8 more
doaj   +1 more source

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