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Figure
1.10 : Map of normal faults in part of the Oseberg Field in the
northern North Sea based on the structural separation of the base of the
Brent formation. Wells #8 and #10 penetrate the producing reservoir and
data from these wells suggest the Omega North and Omega South regions are
isolated from one another by sealing faults. The dashed square indicates
the area of faulting investigated by modeling. Inset: Schematic vertical
cross section that illustrates how the width of the fault stripe on the
map (gray on cross section) depends upon the dip of the normal fault and
the dip separation of a particular horizon. Reprinted from (Maerten et al.,
2000) by permission of the AAPG whose permission is required for further
use. |
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