Next: Artman: REFERENCESPassive seismic imaging
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The correlation of the geophone time series outputs a volume that is
roughly equivalent to the raw data of conventional seismic
acquisition. The parallel code to manufacture this output volume is
almost running. The road ahead is a long one that will involve
velocity estimation, converted wave problems, noise suppression and
separation, simultaneous inversion of multiple experiments, and
migration- in short: the rest of the field of modern seismic data
processing.
Before all of these issues are addressed however, one of the principal
problems to be addressed is that of the separation of the direct
incident Wave field from that reflected from the free surface. This
will be my principal goal in the short term. Some preliminary ideas
for this are outlined in ().
Assuming positive results, the next step will be to identify a
location and acquisition strategy for SEP to collect its second
passive seismic dataset as suggested in ().
Next: Artman: REFERENCESPassive seismic imaging
Up: Prucha and Biondi: STANFORD
Previous: Santa Clara Valley Seismic
Stanford Exploration Project
6/7/2002