The second webinar in a four-part series explains the benefits of an increased range of both temporal frequencies and spatial frequencies for higher seismic resolution.
What level of background knowledge is assumed?
Basic knowledge of the reflection seismic method is required, but there is no math involved and we’ve tried to cut jargon that can alienate non-specialists. Some basic seismic processing knowledge would also be useful, but everything is explained with illustrations and examples.
Topic: Temporal and Spatial Sampling | Speaker: Andrew Long, PGS | Duration: 10 minutes
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