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AAPG Bulletin


AAPG Bulletin, V. 90, No. 5 (May 2006), P. 735-752.

Copyright copy2006. The American Association of Petroleum Geologists. All rights reserved.


Seismic facies and reservoir characteristics of a deep-marine channel belt in the Molasse foreland basin, Puchkirchen Formation, Austria

Menno J. De Ruig,1 Stephen M. Hubbard2

1Rohoumll-Aufsuchungs A.G., Schwarzenbergplatz 16, A1015 Vienna, Austria; present address: Shell International Exploration and Production, Kesslerpark 1, 2288 GS Rijswijk, Netherlands; [email protected]
2Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305; [email protected]


Oligocene–Miocene deep-water deposits of the Puchkirchen and basal Hall formations contain the main gas reservoirs of the Austrian Molasse Basin. A new seismostratigraphic model, based on a 2000-km2 (772-mi2), regional, three-dimensional (3-D) seismic data set, has fundamentally changed our understanding of the depositional processes and reservoir distribution in this classic deep-water foreland basin.

Regional 3-D seismic attribute maps, calibrated by nearly 350 wells, reveal that sedimentation occurred primarily within the confines of a large (3–5 km [1.8–3.1 mi] wide by gt100 km [gt62 mi] long), low-sinuosity channel belt that occupied the Molasse Basin foredeep. The channel fill consists predominantly of turbiditic conglomerate and sandstone, as well as chaotic slump and debris-flow deposits. Overbank areas are characterized by fine-grained turbiditic sandstone and mudstone. Incised canyons and ponded slope fans were active along the southern basin margin; lateral tributary channels intersected the axial channel belt in the north. Significant accumulations of gas are stratigraphically and structurally trapped in channel thalweg and slope-fan sandstones, with more modest amounts in overbank lobe and tributary-channel deposits.

Basin geometry had a profound effect on the architecture of the channel belt and subsequent sediment distribution. Large-scale deep-water channel systems are poorly documented from foreland basins; the depositional model developed for the Puchkirchen Formation was made possible through the use of high-quality seismic data and an extensive drill-core database. The depositional model may be a useful analog for other elongate, deep-water basins, especially those that lack extensive, modern data sets.

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