Imaging of Steep
Salt
Face and Surrounding Sediments Using
Vertical
Seismic Profile (VSP)
Converted Waves
Li, Yingping, Xiaomin Zhao, Fran
Doherty, VSFusion, A Baker
Hughes-CGG Company,
In the Gulf of Mexico, North Sea, and
salt
bodies. Accurately
mapping
subsurface
salt
flank
and sub-
salt
structures are critical tasks for
exploration and reservoir characterization. The steep sides of a
salt
dome
with
irregularly shapes are hard to image with adequate accuracy by using surface
seismic alone. Thus, VSP surveys with 3C receivers in a wellbore
are usually requested for improving images of reservoir structures.
In this paper,
an offset VSP (OVSP) and a refraction
salt
proximity (SP), simultaneously
acquired in
Salt
Basin
salt
boundary and updip
sediment reflectors. Both transmitted P-P and P-S converted waves from the SP
survey were used to calculate 3D
salt
exit points which delineate the steep
salt
face. Furthermore, we developed a robust method to estimate Vp/Vs ratios in the sedimentary rocks flanking the
salt
dome
. Reflected waves PP and PS conversion, from the steep
salt
interface and updip sediment reflectors, were separated from 3C OVSP data
and depth migrated to obtain their images, using a velocity model from a check
shot and the estimated Vp/Vs ratio. The migrated
images using both PP and PS converted waves provide a precise definition of
the steep
salt
face and reservoir sands flanking the
salt
dome
. This study also
indicates that both reflection and reflection surveys can provide a consistent
location of the steep
salt
flank
, demonstrating the strength of combining these
VSP techniques.