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Think for instance about how many earthquakes happen on a given fault segment during a certain interval of time.
To relieve the on-line computation load, the fault origins considered in diagnosis are limited to the basic events in the cut sets of a given fault tree.
"It's true that you can't have an earthquake larger than a given fault can provide," said Serge Shapiro, a professor at the Free University of Berlin who has studied what scientists refer to as induced seismicity.
For a given fault dip and slip rate, growth-strata geometries are strongly influenced by the fault-propagation to slip ratio (p/s) and the width of the zone of distributed deformation.
However, multiple circulation events recorded along a given fault segment deserve to be studied in minute detail in order to unravel the chronology of these events, precipitation processes and associated mechanisms.
Significantly, the permeability along any given fault can vary, section-wise.
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This is accomplished through the design of an appropriate nonlinear control law based on feedback linearization that allows isolating given faults by effectively decoupling the dependency between certain process state variables.
Based on different mathematical principles and modes, the sealing properties of one or more given faults are quantitatively identified and predicted by considering various sealing mechanisms and factors.
Although this excavation exposed hundreds of meters of section, the structural complexity caused by extensive faulting has obscured the stratigraphic relationships between the various formations, such that only a portion of one, or at most two, formations are present in any given fault-bounded block (Figure 3).
This gave fault slip rates from 0.29 to 0.16 mm/year (DMR, 2009b).
We propose an efficient computational approach to determine the achievable fault signatures for a given additive fault model.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com