Reservoir Characterization of the Wilcze Field, Foresudetic Monocline, Western Poland

K. J. Head; J. D. Card; J. Twyman; G. Jobidon

doi:10.3997/2214-4609.201409737

f Reservoir Characterization of the Wilcze Field, Foresudetic Monocline, Western Poland
By K. J. Head, J. D. Card, J. Twyman and G. Jobidon
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 57th EAGE Conference and Exhibition, May 1995, cp-90-00544
ISBN: 978-90-73781-06-1
DOI: https://doi.org/10.3997/2214-4609.201409737

Abstract

The Permian Zechstein Formation of the Fore-Sudetic Monocline of Western Poland is characterized by rapid lateral facies changes from dolomite to anhydrite or halite. The share velocity contrast related to these facies changes causes apparent faulting of seismic horizons within both the Zechstein reservoir and the underlying Rotliegendes reservoir. Conventional seismic interpretation showed a three way structurally closed anticlinal field, with questionable closure in the fourth direction.

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1995-05-29

2024-04-25

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f Reservoir Characterization of the Wilcze Field, Foresudetic Monocline, Western Poland

Abstract

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