SNU Big Data Knowledge Information Platform
Full Menu
AI
Your Browsing History
10 More
loading...
Report registration
Paper List
Evolution of slip susceptibility of Quaternary faults in southeastern Korea from Quaternary to present day
Author
김지연, 장찬동
Journal Title
Geosciences Journal
Publication Year
2021
Topics
Summary
This study analyzes the geomechanical stability of Quaternary active faults in southeastern Korea to investigate their present-day activity. By estimating stress states based on Quaternary fault data and current earthquake mechanisms, and using slip tendency and fault instability indices, the slip susceptibility of the faults was evaluated. The results show an increase in slip susceptibility for most Yangsan Faults and some Ulsan Faults.
Related Content
LikeSNU analyzes your query semantically to recommend related resources.
-
The mechanics of earthquakes and faulting
-
Contemporary lithospheric motion seismic geology : proceedings of the 30th International Geological Congress, Beijing, China, 4-14 August 1996, volume 5
-
Meso-scale shear physics in earthquake and landslide mechanics
-
hillslope form and process
-
Stress evolution and fault stability during the Weichselian glacial cycle
-
The internal structure of fault zones : implications for mechanical and fluid-flow properties
-
Geotechnical slope analysis
-
Rock fractures in geological processes
-
Problems and solutions in structural geology and tectonics
-
Reconstructing Quaternary environments
-
Earthquake thermodynamics and phase transformations in the earth's interior
-
Evolution of geological structures in micro- to macro-scales
-
Mechanics problems in geodynamics
-
Geology of the earthquake source : a volume in honour of Rick Sibson
-
Earthquake and volcano deformation
-
Fault zone dynamic processes : evolution of fault properties during seismic rupture
-
Tectonic geomorphology
-
Elastic wave propagation : proceedings of the second I.U.T.A.M.-I.U.P.A.P. Symposium on Elastic Wave Propagation, Galway, Ireland, March 20-25, 1988
-
Tectonic and stratigraphic evolution of Zagros and Makran during the Mesozoic-Cenozoic
-
Triassic-Jurassic rifting : continental breakup and the origin of the Atlantic Ocean and passive margins
Previous
Next
Previous
Next