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The main objectives of the interpretation of seismic data are:

- structural building surfaces, oil and gas facilities, including the correlation of horizons, tracing faults, building velocity model;

- prediction of the geological section, providing for the identification of conditions of sedimentation, distribution reservoirs and reservoir properties.

An important step in the seismic interpretation is
determine whether the seismic time section geology

Binding reflectors of the seismic data logging seysmofatsionny analysis
Binding reflectors of the seismic data logging seysmofatsionny analysis

To seismostratigraphic dismemberment of the wave field and its identification with the geological boundaries of geoacoustic modeling is performed based on the AK with the assistance of information on LOG. A comparison of synthetic routes to the actual reliability characterizes seismostratigraphic binding

Selection of a model based on seismic wavelet AK. Binding to the geological cross-section

Selection of a model based on seismic wavelet AK. Binding to the geological cross-section

Study of the geological structure is satisfied on the basis of studies of core samples, interpretation, LOG, seismic data

Structural map of reflecting horizonIIa (sole Bazhenov)

Structural map of reflecting horizonIIa (sole Bazhenov)

Type of the section of the upper part of the Paleozoic rocks

Type of the section of the upper part of the Paleozoic rocks

Predicting variation in lithology of carbonate rocks

Regional tectonic model

Structural map of reflecting horizonIIa (sole Bazhenov)

Archinskoye, Urmanskoye lift located within the erosion-tectonic units, slightly raised above the erosion surface, which did not contribute to the formation of strong weathering crusts.

Archinskoye, Urmanskoye lift located within the erosion-tectonic units, slightly raised above the erosion surface, which did not contribute to the formation of strong weathering crusts.

Next - new technology for processing and interpretation