Removal of opacity

ADVERTISEMENT
From SEG Wiki
Jump to: navigation, search
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


Figure 7.5-7a shows a horizontal slab of about 100 ms in thickness isolated from a 3-D poststack time-migrated volume of data. The amplitudes within the slab were actually manipulated to enhance the structural and de-positional features. Amplitude manipulation involves suppressing a range of positive and negative amplitudes below a specified threshold value so as to remove the opacity effect caused by the suppressed amplitudes. The same slab with labeled depositional features is shown in Figure 7.5-7b. Among the features identified are a carbonate shelf, the shelf edge, a channel system, and two submarine fan lobes. The color indicates the seismic amplitudes retained in the slab. Figure 7.5-7b is a product of what interpretive work means — a description of the depositional environment.

To demonstrate that interpretation is not just picking a set of time horizons, but it is more what you do after picking, consider the data set in Figure 7.5-8. We see a sample time slice (Figure 7.5-8a), a crossline (Figure 7.5-8b) and an inline (Figure 7.5-8c). The objective is to identify sand dunes which are confined between horizons T6 and T8. None of the conventional displays in the form of cross-sections of the image volume as shown in Figure 7.5-8 can provide a rapid identification of the sand dunes.

Start with the entire image volume and isolate a time slab bounded by the time horizons T6 and T8 as labeled in Figures 7.5-8b,c. Then, remove opacity to enhance the series of sand dunes as shown in Figure 7.5-9a. A vertical cross-section of the slab with the individual sand dunes is shown in Figure 7.5-9b.

An interpretation of a deltaic sequence is made possible by 3-D visualization and amplitude manipulation. Figure 7.5-10a shows the sequence under consideration highlighted on a vertical cross-section from a time-migrated volume of data. Figure 7.5-10b shows the isolated deltaic sequence with the individual members of the sequence identified by removing opacity from the subvolume that includes the deltaic sequence highlighted in Figure 7.5-10a.

See also

External links

find literature about
Removal of opacity
SEG button search.png Datapages button.png GeoScienceWorld button.png OnePetro button.png Schlumberger button.png Google button.png AGI button.png