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File:Vol.6 F1.22.jpg
Vol.6_F1.22.jpg (766 × 393 pixels, file size: 49 KB, MIME type: image/jpeg)
An example of sparse-spike inversion results. The results of trace inversion can be used to identify spatially distinct bodies with specific impedance ranges. This example is of the same area of the Gulf of Mexico as shown in Fig. 1.3, but after a sparse-spike inversion routine has been performed and the lowest-impedance areas selected as individual bodies. In this area, virtually all these bodies are hydrocarbon reservoirs, although not all are large enough to be economically produced. The two reservoirs identified by A and B in Fig. 1.3 are also identified here. (Data provided by Diamond Geophysical through the Energy Research Clearing House; figure prepared by J.I. Haataja.)
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 20:10, 10 December 2012 | | 766 × 393 (49 KB) | Glenda Smith (Glendasmith) (talk | contribs) | An example of sparse-spike inversion results. The results of trace inversion can be used to identify spatially distinct bodies with specific impedance ranges. This example is of the same area of the Gulf of Mexico as shown in Fig. 1.3, but after a spar... |
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