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Identification of seismic anomalies caused by gas saturation on the basis of theoretical P and PS wavefield in the Carpathian Foredeep, SE Poland

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The thin-layer build of the Carpathian Foredeep Miocene formations and large petrophysical parameter variation cause seismic images of gas-saturated zones to be ambiguous, and the location of prospection wells on the basis of anomalous seismic record is risky. A method that assists reservoir interpretation of standard recorded seismic profiles (P waves) can be a converted wave recording (PS waves). This paper presents the results of application of a multicomponent seismic survey for the reservoir interpretation over the Chałupki Dębniańskie gas deposit, carried out for the first time in Poland by Geofizyka Kraków Ltd. for the Polish Oil and Gas Company. Seismic modeling was applied as the basic research tool, using the SeisMod program based on the finite-difference solution of the acoustic wave equation and equations of motion. Seismogeological models for P waves were developed using Acoustic Logs; S-wave model (records only from part of the well) was developed on the basis of theoretical curves calculated by means of the Estymacja program calibrated with average S-velocities, calculated by correlation of recorded P and PS wavefields with 1D modeling. The conformity between theoretical and recorded wavefields makes it possible to apply the criteria established on the basis of modeling for reservoir interpretation. Direct hydrocarbon indicators (bright spots, phase change, time sag) unambiguously identify gas-prone layers within the ChD-2 prospect. A partial range of the indicators observed in the SW part of the studied profile (bright spot that covers a single, anticlinally bent seismic horizon) points to saturation of the horizon. The proposed location is confirmed by criteria determined for converted waves (con-tinuous seismic horizons with constant, high amplitude) despite poorer agreement between theoretical and recorded wavefields.
Czasopismo
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191--208
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autor
  • Department of Geophysics, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Al. Mickiewicza 30, 30-059 Kraków, Poland, pietsch@agh.edu.pl
Bibliografia
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  • Dziadzio, P., 2000, Depositional sequences in the Badenian and Sarmatian formations in SE part of the Carpathian Foredeep, Prz. Geol. 48, 12, 1124-1138 (in Polish).
  • Dziadzio, P., B. Liszka, A. Maksym, E. Masłowski and G. Staryszak, 1997, Autochtonic Miocene sedimentation medium in the marginal zone of the Carpathians and geologicaldepositional interpretation in the Husów-Albigowa-Krasne region, Proc. Conf. "Complex Geological Analysis - a Source of Progress in Petroleum Prospecting", Warszawa, 157-170 (in Polish).
  • Ensley, R.A., 1985, Evaluation of direct hydrocarbon indicators though comparison of compressional-and shear-waves seismic data: A case study of the Myrnam gas field, Alberta, Geophysics 50, 1, 37-48.
  • Frankowicz, E., 2004, Seismic modelling as a tool for verifying the correctness of seismostratigraphic interpretation, Reports of the Meeting of Scientific Committee of the Polish Academy of Sciences 48 (in Polish).
  • Frankowicz, E., K. Pietsch and S. Porębski, 2005, Seismic modeling applied to identification of sandstone lithosomes (Carpathian Foredeep). Proc. of EAGE 67th Conf., Madrit, p. 168.
  • Górka, A., K. Madej, A. Maksym and P. Gliniak, 2004, Main directions for hydrocarbon prospecting in southern Poland, Proc. of the Conf. GEOPETROL 2004, Prace INiG 130, 55-58 (in Polish).
  • Graves, R.W., 1996, Simulating seismic wave propagation in 3D elastic media using staggered grid finite differences, Bull. Seism. Soc. Am. 86, 1091-1106.
  • Gruszczyk, E., P. Misiaczek, G. Kwaśny and Z. Trześniowski, 2002, Multicomponent seismic case history - Carpathian Foredeep area, Zbiornik Prednasok, Technika Universita v Kosicach, 42-47.
  • Gruszczyk, E., Z. Trześniowski, P. Misiaczek, P. Brettwood and J. Tessman, 2003, Chałupki Dębniańskie field: Improving drilling success in shallow gas reservoirs with VectorSeis, First Break 21, February, 37-43.
  • Kelly, K.R., R.W. Ward, S. Treitel and R.M. Alford, 1976, Synthetic seismograms: A finitedifference approach, Geophysics 41, 1, 2-27.
  • Maksym, A., B. Liszka, G. Staryszak and P. Dziadzio, 1997, Sedimentation model of the Badenian-Sarmatian sandstone formations (autochtonc Miocene, the Husów-Albigowa-Krasne region), Proc. Conf. "Complex Geological Analysis - a Source of Progress in Petroleum Prospecting", Warszawa, 171-174 (in Polish).
  • Marzec, P., M. Kobylarski, K. Pietsch and T. Danek, 2004, Efficiency of seismic modeling programs based on the wave and ray theory of seismic wave propagation, Proc. of the Conf. GEOPETROL 2004, Prace INiG 130, 209-214 (in Polish).
  • Pietsch, K., and P. Krzywiec, 1994, Facial seismic analysis of the Miocene sediments of the Carpathian Foredeep, Proc. of the First Conf. "Seismic Interpretation Problems", Mogilany, 172-186 (in Polish).
  • Pietsch, K., and R. Hodiak, 1999, Criteria of depositional interpretation of seismic data in eastern part of the Carpathian Foredeep, Proc. Conf. "Geophysics in Geology, Mining and Environmental Protection", Kraków, 75-92 (in Polish).
  • Pietsch, K., and J. Jarzyna, 2002, Identification of Miocene gas deposits in SE part of Carpathian Foredeep from seismic data, Geological Quarterly 46, 4, 449-461.
  • Pietsch, K., D. Dereń and T. Gąsiorowski, 1998, Seismic anomalies caused by multi-horizon gas deposits in NE part of the Carpathian Foredeep, Prz. Geol. 46, 8, 676-684 (in Polish).
  • Pietsch, K., S. Porębski and R. Hodiak, 1999, Seismic representation of Miocene deep-marine depositional system in the Carpathian Foredeep, SE Poland, Proc. of EAGE 61-st Conf., Helsinki, 5-52.
  • Porębski, S., K. Pietsch and E. Frankowicz, 2004, Seismic expression of craton-fed turbidite gas-reservoirs in the Carpathian Foredeep (Miocene, Poland), EAGE 66th Conference,
  • Exhibition - Paris, 7-10 June, Extended Abstracts, 4 pp. (in Polish).
  • Yang, D.H., E. Liu, Z.J. Zhang and J. Teng, 2002, Finite-difference modeling in twodimensional anisotropic media using a flux-corrected transport technique, Geophys. J. Int. 148, 320-328.
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Bibliografia
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bwmeta1.element.baztech-article-BSL7-0021-0018
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