| 摘要 |
A method of imaging a subterranean formation. The method includes emitting a primary wave from a source point, such that a portion of the primary wave travels into the subterranean formation and is refracted along a geologic layer in the subterranean formation and then emitted as a secondary wave from a refraction point on a boundary between the geologic layer and another geologic layer. The method also includes allowing a portion of the secondary wave to be reflected from a first reflection point as a tertiary wave. The method further includes allowing a portion of the tertiary wave to be reflected from a second reflection point as a quaternary wave, and collecting data about the quaternary wave at an observation point. |
