Results 81 to 90 of about 175,835 (218)
Active Tectonics of the Eastern and Southern Alps ‐ Crustal Response to Deep Processes? A Review
Abstract Owing to the low N‐S convergence rates between Adria and Europe, crustal deformation rates in the Alps and its forelands are low. Active tectonics are, therefore, difficult to study, especially as non‐tectonic landscape forming processes can erase or modify the tectonic surface imprint. Large‐scale and dense seismological data recently offered
Christoph Grützner +20 more
wiley +1 more source
Abstract Routine Synthetic Aperture Radar (SAR) acquisitions from the Sentinel‐1 constellation enable monitoring of slow surface deformation (millimeters to centimeters per year), yet consistent and accessible pathways for producing validated, user‐ready velocity products remain limited.
Simran S. Sangha +3 more
wiley +1 more source
A Terrain classification system for coseismic landslide hazard analysis: Lebanon, a case study
Coseismic landslides have caused vast amounts of damage throughout history, and are often responsible for more damage than all other seismic hazards combined (Kramer, 1996).
Wartman, Joseph +2 more
core +1 more source
Objective On December 18, 2023, an MS 6.2 earthquake occurred in Jishishan County, Gansu Province, China. Coseismic geological hazards induced by the earthquake crucially threatened the safety of personnel and property.
LIU Shuai +13 more
doaj +1 more source
Abstract Temporal changes in seismicity rates can be conceptually understood as a response and consequence of stress changes. Dieterich (1994, https://doi.org/10.1029/93JB02581) formalized this relationship using empirically derived rate‐and‐state friction laws, and Heimisson and Segall (2018, https://doi.org/10.1029/2018JB015656) later generalized the
Y. Jiang, D. T. Trugman, P. J. González
wiley +1 more source
Abstract Uplifted Pleistocene marine terraces in the Illapel area along the forearc of central Chile record spatially and temporally variable uplift rates on glacial‐cycle timescales. However, the underlying mechanisms for this uplift variability and its potential relationship with the megathrust‐earthquake cycle remain poorly understood.
Roland Freisleben +8 more
wiley +1 more source
Abstract Forward and inverse modeling techniques are often applied to paleotsunamis to reconstruct inundation parameters. The accuracy of both types of models can be influenced by geomorphology, particularly in areas such as northern Cascadia, where rocky headlands and fjords influence tsunami flow and the preservation of sedimentary deposits ...
Stephen E. Bartlett +11 more
wiley +1 more source
Abstract The 1906 Manas Earthquake is the largest earthquake recorded in the Borohoro Shan (BRS) since 1900. The reported magnitude ranges from 7.2 to 8.3, but uncertainties remain regarding its size, mechanism, and responsible fault. Similar confusion exists for the 1812 Nilke and 1944 Xinyuan Earthquakes, the only other Mw > 7 earthquakes in the NE ...
C.‐H. Tsai +3 more
wiley +1 more source
The coseismic landslides induced by 2023 Jishishan earthquake
<p>This dataset provides coseismic landslide points induced by the M<sub>s</sub> 6.2 2023 Jishishan earthquake, Gansu, China. </p ...
Jin, Jiacheng +3 more
core +1 more source
A physics-based integrated sem-newmark model for regional-scale coseismic landslide assessment
Coseismic landslides are one of the most catastrophic effects of earthquakes. Realistic prediction of coseismic landslides is crucial for the design of key infrastructure and to protect human lives in seismically active regions.
Huang, D., Jin, F., Wang, G.
core

