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UNKNOWN SHOT WAVEFORM

A one-dimensional seismogram $ d(t)$ is unknown reflectivity $ c(t)$ convolved with unknown source waveform $ s(t)$. The number of data points ND$ \approx$NC is less than the number of unknowns NC+NS. Clearly we need a "smart" regularization. Let us see how this problem can be set up so reflectivity $ c(t)$ comes out with sparse spikes so the integral of $ c(t)$ is blocky.

This is a nonlinear problem because the convolution of the unknowns is made of their product. Nonlinear problems elicit well-warranted fear of multiple solutions leading to us getting stuck in the wrong one. The key to avoiding this pitfall is starting ``close enough'' to the correct solution. The way to get close enough (besides luck and a good starting guess) is to define a linear problem that takes us to the neighborhood where a nonlinear solver can be trusted. We will do that first.


Subsections
next up previous [pdf]

Next: Block cyclic solver Up: Claerbout: Blocky models: L1/L2 Previous: BLOCKY LOGS: BOTH FITTING

2009-10-19