Sentence examples for fault was given from inspiring English sources

Based on the seismic profile (Fig. 6) (Cautru 1988, redrawn by Koelbel et al. 2011), the depth of each fault was given.

Namely, because this structure was considered a low-density body that intruded into the high-density layer, the dip of the reverse fault was given by the dip of the minimum eigenvector of the gravity gradient tensor.

As to why the dip of normal fault was given by the dip of the maximum eigenvector of the gravity gradient tensor, I considered that the lower part of the boundary structure (fault) exists inside the low-density area more than its upper part.

As to the reason why the dip of reverse fault was given by the minimum eigenvector of the gravity gradient tensor, I considered that the lower part of the boundary structure (fault) exists inside the high-density area more than its upper part.

Therefore, because the gravity gradient tensor is most sensitive to the subsurface structures near the surface, the structure shown in Fig. 5a was considered a high-density body that intruded into the low-density layer, and the dip of the normal fault was given by the dip of the maximum eigenvector.

Some recommendations for the fastest detection of the fault are given.

First, the synthesis of fault isolation filter and the communication sequence that ensures the isolability of fault is given.

Based on this model, the necessary and sufficient condition on the stochastic stability of networked control system with random delays and actuator fault is given, and the corresponding dynamic output controller design procedure is proposed via the cone complementarity linearization method.

Often the efficient standard of fault is given only to those who do economics without really trying.

In addition, when the length, width, and slip amount of the finite rectangular fault are given, the seafloor deformation is calculated using the Okada's formula (Okada 1985) with assuming a homogeneous half-space.

Length (L), width (W), and slip amount (D) of a finite rectangular fault are given by these scaling laws using the M w a,b The initial tsunami height conditions of src01, src02, src03, and src04 shown in figures are yielded by the pairs of FP1/SC1, FP1/SC2, FP2/SC1, and FP2/SC2, respectively c The tsunami data stations are shown in Fig. 2.