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Now suppose there was an explosion at t = 0,
a half-strength implosion at t = 1,
and another, quarter-strength explosion at t = 3.
This sequence of events determines a ``source'' time series,
.The Z-transform of the source is
.The observed yt for this sequence of explosions and implosions
through the seismometer has a Z-transform Y(Z), given by
| ![\begin{eqnarray}
Y(Z) &\eq & B(Z) - {Z \over 2}\, B(Z) + {Z^3 \over 4}\, B(Z) \n...
...2} + {Z^3 \over 4} \right)\, B(Z) \nonumber \\ &\eq & X(Z)\, B(Z)\end{eqnarray}](img15.gif) |
|
| |
| (4) |
The last equation
shows polynomial multiplication as the
underlying basis of time-invariant linear-system theory,
namely that the output Y(Z) can be expressed as the input X(Z) times
the impulse-response filter B(Z).
When signal values are insignificant
except in a ``small'' region on the time axis,
the signals are called ``wavelets.''
Next: Convolution equation and program
Up: SAMPLED DATA AND Z-TRANSFORMS
Previous: Linear superposition
Stanford Exploration Project
3/1/2001