Fig. 22.6 Overview of a typical model construction work flow.
Seismic interpretation is usually done in time domain and depthconverted (steps a–d). Isochore maps are made and merged
with the seismic framework to make the geological framework
(step e). An optional test grid may be made for quality control
(step f). Based on this, two more 3D grids are made (steps g, h),
which are filled with properties (steps i, j)
566
J.C. Rivenæs et al.
Seismic interpretation is usually done in time domain and depthconverted (steps a–d). Isochore maps are made and merged
with the seismic framework to make the geological framework
(step e). An optional test grid may be made for quality control
(step f). Based on this, two more 3D grids are made (steps g, h),
which are filled with properties (steps i, j)
566
J.C. Rivenæs et al.
