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In future work, the experiment can be designed with multiple faults, such as the crack with bearing fatigue, oil-film force, or rub-impact fault to study the influence of other faults on the dynamics of cracked rotor systems and the crack detection method in multi-fault cases.
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In order to re-evaluate the topographic, tectonic and climatic influences on erosion, we adopted five parameters (slope, mean local relief, historical cumulative seismic moment, runoff coefficient of variation and fault density) to study 11 drainage basins in north-east Tibet.
Based on the fault diagnosis theory, this paper proposes a robust fault diagnosis method to study the fault diagnosis problem of MMC-HVDC systems.
We analyze data collected from 2001 to 2012 at 22 campaign GPS sites that were designed to measure displacements along the faults and to study present-day tectonic deformation in NWV (Fig. 2).
The dextral-reverse Pusteria and Sprechenstein-Mules Faults (Italian Eastern Alps) provide an opportunity to study fault rocks and damage distribution as a function of host-rock lithology and fabric, and of fault geometry.
Guo and Morgan (2008) simulated the breakdown of fault blocks using PFC2D to study the frictional strength, mechanical behaviour and stress and strain rate of evolving fault gouge and their dependence on normal stress and uniaxial compressive strength.
This article can be useful to the upcoming scenario designers and seismologists in their quest to study fault parameters.
This paper builds on this travelling wave-based approach to study fault behaviour in bipolar, asymmetrical and symmetrical monopolar systems.
However, this phenomenon is generally neglected (except in inversion models) in analogue and numerical models performed to study fault network growth.
This paper proposes the use of an FPGA-based fault injection technique, AMUSE, to study the effect of malicious attacks on cryptographic circuits.
The Nojima Fault Zone Probe was designed to study the properties and healing processes of the Nojima fault, which is the surface fault rupture of the Hyogo-ken Nanbu earthquake (M7.2) of 1995 19955 Kobe earthquake).
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