Results 11 to 20 of about 2,065,188 (309)

A study of the influence of the crossing-slope fault geometry on the slope seismic response

open access: yesShuiwen dizhi gongcheng dizhi, 2023
Compared with the landslides in the general gravity environment, the earthquake-induced landslides are significantly different in formation mechanisms and kinetic characteristics.
Zhimin WANG   +4 more
doaj   +1 more source

Irregular rupture propagation and geometric fault complexities during the 2010 Mw 7.2 El Mayor-Cucapah earthquake

open access: yesScientific Reports, 2022
The 2010 M W 7.2 El Mayor-Cucapah, Mexico, earthquake ruptured multiple faults with different faulting mechanisms. Resolving the earthquake rupture process and its relation to the geometric fault complexities is critical to our understanding of the ...
Shinji Yamashita, Yuji Yagi, Ryo Okuwaki
doaj   +1 more source

Quantifying Natural Fault Geometry: Statistics of Splay Fault Angles [PDF]

open access: yesBulletin of the Seismological Society of America, 2009
Abstract We propose a new approach to quantifying fault system geometry, using an objective fit of the fault geometry to a test function, specifically here a fault branch. Fitting a Y-shaped object using a cost function to dextral faults in California, we find a number of significant results arising from use of a a systematic, objective, quantitative ...
R. Ando, B. E. Shaw, C. H. Scholz
openaire   +1 more source

Fault Geometry and Slip Distribution of the 2013 Mw 7.7 Balochistan Earthquake From Inversions of SAR and Optical Data

open access: yesJournal of Geophysical Research: Solid Earth, 2020
The 2013 Mw 7.7 Balochistan earthquake ruptured the Hoshab fault (Pakistan) over 200 km. It was dominated by left‐lateral slip, with a secondary reverse component.
B. Lauer, R. Grandin, Y. Klinger
semanticscholar   +1 more source

Seismic analysis of the Xiluodu reservoir area and insights into the geometry of seismogenic faultsKey points

open access: yesEarthquake Science, 2022
The Xiluodu (XLD) reservoir is the second largest reservoir in China and the largest in the Jinsha River basin. The occurrence of two M > 5 earthquakes after reservoir impoundment has aroused great interest among seismologists and plant operators.
Hongfu Lei   +5 more
doaj   +1 more source

Fault slip envelope: a new parametric investigation tool for fault slip based on geomechanics and 3-D fault geometry [PDF]

open access: yesSolid Earth, 2019
By combining a 3-D boundary element model, frictional slip theory, and fast computation method, we propose a new tool to improve fault slip analysis that allows the user to analyze a very large number of scenarios of stress and fault mechanical property ...
R. Soliva   +3 more
doaj   +1 more source

Major California faults are smooth across multiple scales at seismogenic depth

open access: yesSeismica, 2023
Surface traces of earthquake faults are complex and segmented on multiple scales. At seismogenic depth the detailed geometry of faults and earthquake rupture is mainly constrained by earthquake locations.
Anthony Lomax, Pierre Henry
doaj   +1 more source

Physical mechanism for severe seismic hazard in the 2010 Yushu, China, earthquake (Mw= 6.9): insights from FEM simulations

open access: yesGeomatics, Natural Hazards & Risk, 2020
The moderate-size 2010 Yushu earthquake (Mw 6.9) caused severe seismic damage around the source region which is situated on the sparsely populated hinterland of the Tibetan Plateau. But until now the mechanisms have not been well understood. To this end,
Shoubiao Zhu, Jie Yuan
doaj   +1 more source

Fault geometry and kinematics of the 2021 Mw 7.3 Maduo earthquake from aftershocks and InSAR observations

open access: yesFrontiers in Earth Science, 2022
The 2021 Mw 7.3 Maduo earthquake revealed the significant seismic hazard of faults developed within the Bayan Har Block of eastern Tibet, China (e.g., the Kunlun Pass–Jiangcuo Fault).
Xiaoran Fan   +6 more
doaj   +1 more source

Source Model and Stress Disturbance of the 2017 Jiuzhaigou Mw 6.5 Earthquake Constrained by InSAR and GPS Measurements

open access: yesRemote Sensing, 2018
Seismogenic fault geometry, especially for a blind fault, is usually difficult to derive, based only on the distribution of aftershocks and interference fringes of Interferometric Synthetic Aperture Radar (InSAR).
Shunying Hong   +8 more
doaj   +1 more source

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