Records have been obtained by well-to-well seismic propagation, shooting primacord charges into one well, and locking geophones into other wells several hundred meters away. Seismic arrivals containing a large amount of information have been recorded and analyzed by an iterative ray-tracing technique. If the conditions are favorable, significant wave speed transition zones and small structures can be detected between wells.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.