Abstract
Refraction surveys are a well-established method of imaging subsurface velocities, both in terms of the deep crustal structure at global scales and in the shallow near surface. These surveys generally involve deploying an array of receivers on the surface (or water bottom) and recording arrivals from a seismic source initiated at or near the surface.
Original language | English (US) |
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Pages (from-to) | 546-550 |
Number of pages | 5 |
Journal | The Leading Edge |
Volume | 30 |
Issue number | 5 |
DOIs | |
State | Published - May 2011 |