Sentence examples for fault length from inspiring English sources

This observation affects the various faulting parameters which include fault length, width, depth and average slip.

Fault length is particularly important with larger faults tending to accommodate more strain than smaller faults in a given population.

One suggestion is that static triggering works better when the effects of several — temporally distinct — large earthquakes are superimposed and short-range triggering effects (within one fault length) dominate.

The pulse behavior and the tracer breakthrough curve, as well as their sensitivity to fault dispersion, fault length and fault fluid velocity are analyzed.

This typically leads to overestimate the fault length and the expected magnitude or to the increase in the number of seismogenic sources affecting an area.

As faults lengthen and grow, they interact with features at greater distances and over a broader area, so the potential for tip shielding effects will increase as fault length increases.

Beryllium-10 catchment-wide denudation rates range from 19.9 ± 3.2 to 149 ± 22.5 m/Ma and demonstrate strong correlations with mean catchment slope and with total active fault length normalized by catchment area.

The earthquake hypocenter was 18 km far away with local magnitude 5.8; the fault length was 13.8 km, as recorded by the Egyptian national seismological network (ENSN) at Helwan.

New data is provided on scaling relations between: i) fault length and the length of related fractures; ii) mean step length and width for overstepping fault segments; iii) angular values at the intersection of the fault plane and related fractures.

The amount of slip in each earthquake on the Firouzkuh fault is difficult to estimate, but assuming the entire ∼55 km fault length ruptures in each event, they will have had a maximum magnitude of 7.1.

Small tremors that follow an earthquake are considered aftershocks if they originate within the fault harbouring the earthquake or if they occur outside the fault within one full fault length (the measurement of the fault end to end) from the earthquake's epicentre.