Answers are grounded in this paper and cite their sources.
In the past, survey planning was based mainly on analysis of the acquisition geometry at the surface assuming a symmetric raypath between source and receiver. CMP fold and offset distribution maps were used to compare alternate acquisition geometries. When sources and receivers are at different depths (e.g., for OBS surveys) or when converted waves are considered, this assumption no longer holds, even in a horizontally layered subsurface.
No takes yet. Share an insight, caveat, or question.
Jürgen Hoffmann (2001) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: