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Geological interpretation of seismic sections in structurally and lithofacially complex settings encounters many difficulties connected first of all with a correct identification of seismic horizons and with their correct stratigraphical correlation. In this paper the results of a wavelet analysis and zero-phase section calculation were presented, aimed at the improvement of resolution of a seismic section and identification of the so-called P1 reflection from the top of Rotliegendes. It was found that the improvement of section resolution allows to follow such subtle phenomena as a change of signal shape connected with the water/gas contact. An extracted zero-phase wavelet attributed to the Rotliegendes top allows for certain identification of this seismic horizon.
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Rocznik
Tom
Strony
283--306
Opis fizyczny
Bibliogr. 17 poz.
Twórcy
- Oil and Gas Institute 31-503 Kraków, ul. Lubicz 25a tel. (0-12) 421-06-86, znzwincz@cyf-kr.edu.pl
Bibliografia
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Bibliografia
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bwmeta1.element.baztech-article-BSL4-0002-0004