Geoscience Reference
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Fig. 2.4 A structural build
based on fault sticks from
seismic (a), converted
into a linked fault system
(b), integrated with depth-
converted horizon picks
(c) to yield a conceptually
acceptable structural
framework which honours
all inputs (d). The
workflow can equally well
be followed using time
data, then converting to
depth using a 3D velocity
model. The key feature of
this workflow is the
avoidance of intermediate
surface gridding steps
which are made
independently of the final
interpreted fault network.
Example from the Douglas
Field, East Irish Sea
(Bentley and Elliott 2008 )
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