The results suggest that the sandstone body was a product of a fluvial environment of a special transitional type.
In general, the sandstone body have been deposited by a river, possibly a distributary flowing on a coastal plain.
Sedimentary sandstone body of oxbow istracked and described using horizontal slice and 3D stereo display techniques, and its lithology is studied by analyzingreservoir depth, amplitude and frequency.
Information about this type of sandstone body has not been available until recently.
