The phrase "amount of fault" is correct and usable in written English.
It can be used when discussing the degree or extent of responsibility or blame attributed to someone for a particular situation or outcome.
Example: "In the accident, the investigation revealed that the amount of fault lay primarily with the driver who ran the red light."
Alternatives: "degree of blame" or "level of responsibility".
Seismologists now describe earthquakes using the moment magnitude scale, which is defined by the extent and amount of fault slippage during the earthquake, but can also be calculated from seismograph readings.
Firstly, according to the amount of fault current variation in the beginning of the feeder, the fault location is estimated.
Faults can separate reservoirs into compartments, particularly when a fault offset juxtaposes sandstone against shale or a significant amount of fault gouge within the fault zone during faulting.
Fig. 8 Sum of squared residuals between the observed and calculated values when varying the dip angle of the fault plane and amount of fault slip.
The total amount of fault location estimated errors were combined to generate an error function and an original study about a thorough statistical analysis was performed.
In order to produce coastal uplift of about 3 m (i.e., height of the lowest emergent terraces), a larger amount of fault slip (i.e., 10 m) on the upper-plate fault is modeled and will produce a wave height of more than 5 m along the coasts of Badoc.
The land has been subjected to a considerable amount of faulting, folding, uplifting, and volcanic activity over geologic time, and much of the region is mountainous.
The Hamiltonian during the period t ∈ [t c, t s ] is equal to the amount of fault-related energy that is injected into the system at t = t c.
The most important point affecting the success of BITCP is that the first test cases of test suite find a great amount of faults as demonstrated as in Fig. 7.
Transmission electron microscopy showed the development of an extremely large amount of stacking faults and stacking fault intersections, including ε-martensite plates.
However, this appears to be in contrast to the kinematic slip inversion results based on InSAR (Yarai et al. 2015) and by strong motion records (Asano et al. 2015), which showed that a significant amount of the fault slip actually occurred at the relatively deeper parts of the northern half of the fault rather than that of the southern part.
