Seismic interferometry has become a technology of growing interest for imaging borehole seismic data. We demonstrate that interferometry of internal multiples can be used to image targets above a borehole receiver array. By internal multiples, we refer to all types of waves that scatter multiple times inside the model. These include, for instance, interbed, intrasalt, and water-bottom multiples...

Least-Squares Reverse-Time Migration (LSRTM) is a method that seismologists utilize to compute high-resolution subsurface image. Nevertheless, LSRTM computationally demanding problem. One way reduce the computational costs of choose small region interest and image region. However, finding representations account for wavefields entering target from surrounding boundaries necessary. This paper co...

Marchenko imaging can produce seismic reflection images in which artifacts related to multiples are suppressed. However, in state-of-the-art implementations, multiples do not contribute to the imaged reflectors. With an “event-byevent” deconvolution imaging approach, it is possible to use multiples in Marchenko imaging. We illustrate this for a 1D reflection response in which the primary reflec...