There
is some confusion in the literature and among seismic interpreters when
referring to the thickness of a reservoir in time units. This confusion
results because many people convert bed thickness from distance units
(feet or meters) directly to one-way traveltime across the bed (Fig. 3
below), which is a logical and correct way to define bed thickness in
terms of seismic time.

Figure
3. Distinction between one-way and two-way traveltime thicknesses of
a thin bed. When describing the time thickness of a bed, it is critical
to specify if the time scale is one-way or two-way traveltime, because
there is a factor of 2 difference in these two options for defining
bed thickness.
However,
all time measurements made from seismic reflection data are two-way traveltime
measurements, not one-way traveltime. Thus a bed that is 1.0 ms thick
in one-way traveltime has to be expressed as a 2-ms bed when it is imaged
with a seismic wavelet because the reflection from the base of the bed
involves a downward transmission through the bed (one-way traveltime)
and then an up-going reflection return through the bed (two-way traveltime).
Bed thickness can be defined in terms of either one-way or two-way traveltime
as long as 1. The time scale is defined so that there is no confusion
and 2. Two-way time is always used when bed thickness is being interpreted
from seismic reflection data.
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