The invention discloses a
continuation imaging method suitable for cross-well seismic large-angle reflection conditions. The
continuation imaging method comprises the following steps: when a
direct wave is removed, a
wave field of a seismic source transversely extend towards a wave
detector, and a receiving
wave field of the wave
detector transversely extends towards the seismic source; when the
wave field of the seismic source and the receiving wave field of the wave
detector extend to the same position, related imaging conditions are utilized for transverse
continuation imaging; after images of all shot points are formed, the images are overlapped to obtain an imaging profile for cross-well seismic depth domain migration. The continuation imaging method has the advantages that a large angle of
information dissemination is converted into a small angle in the direction of transverse continuation, so that the imaging effect of a vertical large-angle region is improved; separating an uplink reflected wave from a downlink reflected wave is not needed, so that the
impact of the poor separating effect on an imaging result is avoided; not only the kinematic characteristics (such as
temporal information) of cross-well seismic reflected wave data, but also the dynamic characteristics (such as amplitude information) of the cross-well seismic reflected wave data and the particularity of a cross-well seismic
observation method are considered, so that the continuation imaging method is accurate in imaging and high in precision.