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As an example, fault 1 (F1) in the IEEE 14-node system as shown in Fig. 4 is considered and the coordination working mode is analyzed.
For example, fault tolerance is mainly based on task redundancy, but defining the appropriate level of redundancy is a challenging task.
This work focuses on the design and implementation of a fuzzy inference system for fault detection and isolation (FDI) which can learn from example fault data, and the determination of a suitable optimisation strategy for the membership functions.
Compared to other tectonic settings (for example fault zones in the continental crust, as recently reviewed by Faulkner et al. 2010), studies of fault rocks in subduction zones are still immature.
In this figure, tI and tII are example fault times, tp is the firing instant, (t^{prime}_{text{p}}) is the forward firing instant, t γ is the time corresponding to γmin, and ΔSI and ΔSII are the increased commutating voltage-time areas corresponding to faults at tI and tII respectively.
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For example, fault-free but slow processes can be erroneously added to the list of failed processes.
Groundwater seepages are often found to be in close association with geological and tectonic factors for example, faults, fractures and cavities within the subsurface [6, 9].
For example, faults on both Line-XY and Line-YP are forward faults for relay associated with breaker BXY whereas a fault on Line-XY is in the reverse direction for the relay associated with breaker BYP.
In four examples, faults and folds indicate deformation by glaciotectonism and syndepositional loading.
For example, Byzantine faults (intermittent faults) could be acceptable (Lee and Anderson [1990]; Randell [1975]) whereas other types of faults, such as permanent faults, may be unacceptable.
For example, a fault gouge on the Taiwan Chelungpu fault is 13 cm thick and has a complex structure that includes localized slip zones (Ma et al. 2006; Hirono et al. 2008b).
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