1.Identification of objects and allocation of borders. In the spectral image (a figures 5-8) it is visible, that the Bazhenovsky retinue is divided into some blocks. Borders of blocks are practically vertical, they are clearly visible.
2.Lithology partition. Conformity of a spectrum and lithology is rather mediated. It is impossible co-ordinate color to concrete lithology. But within one complex, it is possible to assume, that color characterizes lithology. Certainly, the data should be shot by one technique and is processed on one count.
3.Allocation of hydrocarbons. The same principles as at lithology partition. If on the studied area there is a binding (a hole with a product), it is possible to use colour of a spectrum as an additional sign of presence of hydrocarbons. Certainly, in similar geological conditions. Hardly probable it is possible a binding on an interval of the Jurassic period without reservations to consider as a positive sign in the Cretaceous complex.
1. Typification and visualization of spectral types of SEGY files.SEGY files.
2. Any change of color.
3. A package processing mode of files.
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