Sentence examples for generating earthquake from inspiring English sources

As part of the rules of each experiment, we have to define the earthquake catalog against which the forecasts will be tested (testing catalog) as well as the earthquake catalog that can be used as input data for generating earthquake forecasts (learning catalog).

Among them, there are methods that use macroseismic intensity data as the major input, which initially were developed during a series of national research projects aimed at generating earthquake risk scenarios (Giovinazzi and Lagomarsino 2004; Bernardini et al. 2008; Meroni et al. 2008a, b).

The earth is moving always, at different rates and speeds, generating earthquakes.

These experimental results suggest that dehydration embrittlement is a viable mechanism for generating earthquakes independent of depth.

The Lembang fault located at northern part of populated Bandung basin is the most conspicuous fault that potentially capable in generating earthquakes.

Three orthogonal components of generated earthquake ground motion are statistically independent from the point of view of practical engineering.

For fragility analysis, the study employed a set of 200 generated earthquake acceleration records compatible with the elastic code design spectrum.

The matrix of correlation coefficients of spectral accelerations of the generated earthquake ground motions closely matches the target spectral correlation matrix predicted by the Next Generation Attenuation Project.

Representative acceleration time histories such as artificially generated earthquake history compatible with design spectrum, ground motion recorded during real earthquake and idealized near-fault ground motion, have been used to analyze the response.

In the fragility analysis, a set of 240 artificially generated earthquake ground motions compatible with the design spectrum selected to represent the variability in ground motion was employed to study nonlinear dynamic responses of the structures before and after retrofit.

Therefore, the coupling at the interface between the inland plate and the PHS is not sufficient to create stress to generate earthquake activity in Kyushu, as pointed out in central Japan by Townend and Zoback (2006).