Results 11 to 20 of about 4,299,358 (286)

Strong Aftershock Study Based on Coulomb Stress Triggering—A Case Study on the 2016 Ecuador Mw 7.8 Earthquake

open access: yesApplied Sciences, 2017
The 2016 Ecuador M 7.8 earthquake ruptured the subduction zone boundary between the Nazca plate and the South America plate. This M 7.8 earthquake may have promoted failure in the surrounding crust, where six M ≥ 6 aftershocks occurred following this ...
Jianchao Wu   +3 more
doaj   +4 more sources

Identifying the most explainable fault ruptured of the 2018 Palu-Donggala earthquake in Indonesia using coulomb failure stress and geological field report

open access: yesGeodesy and Geodynamics, 2020
This study investigates the relation between the Coulomb failure stress of the mainshock with the aftershocks sequence following the 2018 Palu-Donggala earthquake in Indonesia.
Endra Gunawan   +3 more
doaj   +3 more sources

The Mohr–Coulomb criterion for intact rock strength and friction – a re-evaluation and consideration of failure under polyaxial stresses [PDF]

open access: yesSolid Earth, 2016
Darley Dale and Pennant sandstones were tested under conditions of both axisymmetric shortening and extension normal to bedding. These are the two extremes of loading under polyaxial stress conditions.
A. Hackston, E. Rutter
doaj   +5 more sources

The Generalized Mohr-Coulomb Failure Criterion

open access: yesApplied Sciences, 2023
With the construction of supertall buildings such as high earth dams, the linear envelope of the Mohr-Coulomb (M-C) failure criterion fitted to lower confined pressure would significantly underestimate the loading capacity of foundations, causing a huge ...
Dongshuai Tian, Hong Zheng
doaj   +2 more sources

Evolution of Coulomb failure stress in Sulaiman Lobe, Pakistan, and its implications for seismic hazard assessment

open access: yesEarth and Planetary Physics, 2023
In this research work, we present the evolution of Coulomb failure stress (CFS) in the Sulaiman Lobe and its implications for seismic hazard assessment. The Chaman transform fault, ~1,000 km long, is the major active fault that marks the western boundary between Pakistan and Afghanistan on the Indian Plate.
Muhammad Younis Khan
exaly   +3 more sources

Study on Coulomb Stress Triggering of the April 2015 M7.8 Nepal Earthquake Sequence [PDF]

open access: yesInternational Journal of Geophysics, 2016
In April 2015, a M7.8 earthquake occurred less than one month before a M7.3 earthquake near Kodari, Nepal. The Nepal earthquake sequences also include four larger (M > 6) aftershocks. To reveal the interrelation between the main shock and the aftershocks,
Jianchao Wu   +3 more
doaj   +2 more sources

COULOMB STRESS CHANGES DUE TO RECENT ACEH EARTHQUAKES

open access: yesJurnal Penelitian Fisika dan Aplikasinya, 2015
Coulomb stress change analysis has been applied to understand whether the 2013/07/02 (Mw=6.1) has been triggered by 2013/01/21 earthquake (Mw=6.1) the proximity to failure on the Aceh segment of Sumatra Fault Zone (SFZ). We examine the problem of how one
- Madlazim
doaj   +2 more sources

Mohr-Coulomb Failure Condition and the Direct Shear Test Revisited [PDF]

open access: yesActa Polytechnica, 2004
An alternative critical plane orientation is proposed in the Mohr-Coulomb failure criterion for soils with an extreme property. Parameter identification from the direct shear test is extended to incude the lateral normal stress.
P. Řeřicha
doaj   +2 more sources

Spatiotemporal Evolution of Pore Pressure Changes and Coulomb Failure Stress in a Poroelastic Medium for Different Faulting Regimes [PDF]

open access: yesEarth and Space Science, 2021
Abstract Spatial distribution of aftershocks has been explained by the co‐seismic static Coulomb Failure Stress changes (ΔCFS) to some extent. In practice, the earth's crust is porous medium saturated with fluid filling pores, cavities, cracks, and faults.
Miao Miao   +5 more
openaire   +2 more sources

Stress‐field rotation and rooted detachment faults: A Coulomb failure analysis [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 1997
Several well‐known mechanical models have shown that unusual boundary or loading conditions can alter principal‐stress orientations into configurations consistent with low‐angle normal faulting. Such models, however, have not demonstrated whether magnitudes of reoriented stresses are sufficient to initiate and promote slip on low‐angle surfaces.
Stewart Wills, W. Roger Buck
openaire   +1 more source

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