Imaging beneath shallow gas anomalies in the Gulf of Thailand

From SEG Wiki
Jump to navigation Jump to search
ADVERTISEMENT
Seismic Data Analysis
Seismic-data-analysis.jpg
Series Investigations in Geophysics
Author Öz Yilmaz
DOI http://dx.doi.org/10.1190/1.9781560801580
ISBN ISBN 978-1-56080-094-1
Store SEG Online Store


The fifth 2-D case study for structural inversion is from the Gulf of Thailand. This case study deals with the deleterious effect of shallow gas anomalies on a multileveled reservoir zone along growth faults. The velocity-depth model is characterized by near-horizontal layers with structure-independent velocity variations. Shown in Figure 10.5-1 is the CMP-stacked section. The shallow gas anomalies are represented by the high-amplitude piecewise-continuous reflections within the first 500 ms of the section.

The shallow gas anomalies give rise to fluctuations in the stacking velocity field as seen in Figure 10.5-2. For a horizon below the shallow anomaly zone, CMP raypaths at some locations travel through an overburden with laterally varying velocities associated with the shallow gas anomalies. As a result, traveltimes associated with deeper reflections are distorted.

Time migration (Figure 10.5-3) using a smoothed form of the stacking velocity field (Figure 10.5-2) produces a seemingly accurate image of the subsurface. Note, for instance, the fault below CMP 2170 within 1-2 s time window, and the v-shaped structure below CMP 1370. The subsurface appears to be so simple that one may be tempted to convert this section to depth using vertical raypaths and Dix-converted stacking velocities. However, the anomalous behavior of the stacking velocities will cause Dix conversion to yield meaningless interval velocities.

See also

External links

find literature about
Imaging beneath shallow gas anomalies in the Gulf of Thailand
SEG button search.png Datapages button.png GeoScienceWorld button.png OnePetro button.png Schlumberger button.png Google button.png AGI button.png