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Full waveform inversion for detailed geological imaging where standard seismic methods fail due to vertically oriented structures or severe heterogeneity at the near surface.

Passive seismic imaging where the costs of acquiring standard 2D/3D surveys are an issue. As an example, sound coming out from your drilling operations can be turned into an image of the subsurface.

Seismic Interferometry where virtual sources/receivers can be created nearer to a geological target so that a better image of the target can be derived than the standard 2D/3D methods. For example, a borehole VSP experiment can be transformed into a virtual 2D survey to increase the lateral coverage.

Interferometric seismic source location where the seismic activity is large and manual event identification and source location is not an option or building a velocity model for event location isn’t easy due to the complexity of the underground.