The evaluation of velocity uncertainties in Chapter 2 has shown
that
10 m/s
picking errors in the RMS velocity can cause as much as
200 m/s
errors in the interval velocities. Since I have discussed the issue in
more detail in Chapter 2, I simply show these resulting errors
in interval velocity again in Figure
. The solid line represents
the velocity determined from the original RMS velocity. It shows clearly the
velocity increase connected with the presence of hydrate in the sediment
and the subsequent velocity decrease because of the gas saturation.
Picking errors
give rise to the velocities represented by the dashed lines. The errors
can either enhance the anomalous velocity zones in the hydrate and gas layer
(dashed line) or suppress them (double dashed line). It can be imagined that
these velocity trends will produce different estimates of the hydrate and
gas anomalies.
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