The method does not require the fault type to be known, and is applicable to any type of faults.
Generally, in real HVDC projects, γmin is about 7°, and γ0 is about 18°, and if a CF is not caused, Δφ is relatively small for any type of AC fault.
The principle of FEI is applicable to all types of fault components, including positive-, negandve-, and zero-sequence fault components.
Earthquakes have different properties depending on the type of fault slip that causes them (as shown in the figure).
A type of fault activity called block faulting, in which the movement is predominantly vertical, began to form the valley about 30 million years ago.
In 1899, several years after a powerful tsunami struck the Sanriku Coast, a man named Akitsune Imamura correctly inferred the type of fault slip (now called a megathrust event) that generates such waves.
These faults have been referred to by Evamy et al. (1978) as the 'K' type of fault.
In particular, from a given EFSM specification and a selected type of fault, an EFSM with the selected type of faults is derived.
The type of fault is further classified using the value of δi01.
