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Modal transformation is implemented to decompose the coupled three phase equations due to mutual effects into decoupled ones, and hence directly calculating fault distance in each section without iterative processes.
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Two of the calculated fault plane solutions show an oblique normal faulting mechanism.
Figure 3 Comparison of actual BFR composition and calculated fault rock compositions of selected trace elements.
Consequently, the calculated fault position is substation N, thus the fault location method is failed due to the blind spot.
This paper calculates fault current-division factors and assesses earth-grid safety at 17.1/161-kV Chiahui independent power producer (IPP).
To calculate fault plane solutions using first motion polarities (FMP), the Fortran program FPFIT (Reasenberg and Oppenheimer 1985) was used.
Syndepositional fault patterns and activity data are based on 3D seismic interpretations, which were used in combination to calculate fault throw.
Fault data derived from a map published by ESRI and attributed to the USGS (ESRI 2014) were used to calculate fault density for each basin.
A method based on the grid current is proposed to calculate fault current-division factors and the results are compared with the Endrenyi method as well as the current-distribution electromagnetic-grounding and soil-structure analysis (CDEGS) program.
Trace element anomalies of black fault rocks (BFRs; red diamonds and orange squares and triangles) and calculated fault rock compositions (solid and dashed lines, depending on R values) of selected trace elements (Rb, Sr, Cs, Ba, La, Sm, and Pb) at temperatures of 250°C, 300°C, and 350°C.
Since fracture intensity and apertures in Cleebourg increase towards the fault plane, calculated fracture permeabilities follow this same trend.
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