The phrase "absolute fault" is correct and usable in written English.
It is typically used in legal or insurance contexts to describe a situation where one party is entirely responsible for a loss or damage.
Example: "In this case, the court found the defendant to be in absolute fault for the accident, leaving them liable for all damages incurred."
Alternatives: "complete liability" or "total responsibility".
Dc″ is defined as double the fault-parallel ground displacement when the absolute fault-parallel ground velocity is at a maximum (Fukuyama and Mikumo 2007).
Thus, the final fault point is located at 45.078 kM from substation 3, and the absolute error is 0.078 kM.
The Rand study (a summary is on the Web at www.Rand.org) reported that such an option -- known as "absolute no-fault" -- if chosen by half of all drivers, would reduce the average premium in New Jersey by 36percentt, and premiums for the poor by more than half.
The absolute positioning of the fault model for P-Mod is directly tied to the choice of hypocen-ter; the teleseismic P-wave signal relative alignments for the inversion are insensitive to changes of tens of kilometers.
Note that the back-projection approach provides location and timing of relative energy release during an earthquake, but cannot constrain parameters such as dip of the fault or absolute slip (e.g., Ishii et al., 2005, 2007).
Expected changes during the preslip period for years to months prior to an earthquake, when the slip velocity is still minuscule on a linear scale, are about several to several tens percent depending on the absolute level of the fault's strength.
Brewer said spotting a foot fault is "the absolute most no-brainer call there is for an umpire".
A relative deviatoric stress has been estimated from the data of the seismic slip direction that coincides with that of the shear traction acting on the pre-existing fault since its absolute value is not able to be obtained from only slip direction data.
In addition, the absolute strength level of natural faults cannot be constrained directly by seismic or geodetic observations, and it remains an open question (e.g., Brune et al. 1969; Scholz 2002).
