High-Resolution Forward Stratigraphic Modeling of Ca2-Carbonate Platforms ...
Okm
Om
-100 m
-200 m
-300 m
-400m
10 km
20 km
Werra Anhydrite
(A1 )
Fig.27 Ca2 LSW and A2 LST/eTST, East Germany
Acknowledgements
337
PHIL is a trademark of PetroDynamics Inc. (formerly MarcoPolo Software).
BEB Erdgas and Erdal GmbH, Hannover / Germany is thanked for financial and
data support.
Erdoel-Erdgas Gommern GmbH, Gommern / Germany is thanked for providing
data and the permission for publication.
For valuable discussions the authors thank Thomas Aigner, Scott A. Bowman,
Werner Dauben, Chris Kendall, Werner Leu, Eberhard Plein, Ingo Steinhoff and
Walter L. Watney.
We also thank Karen M. Love for her review of this paper.
We gratefully acknowledge the management of BEB Erdgas and Erdoel GmbH,
as well as the W.E.G. publication committee, for permission to publish this paper.
References
Below,A. (1992): Fazies- und geochemische Diagenesestudie im Zechstein 2-Karbonat (Ca2)
Nordwestdeutschlands.- Rep. Geol. Pal. Inst. Univ. Kie1, 60, 147 p.
Fuchtbauer, H. (1964): Fazies, Porositat und Gasinhalt der Karbonatgesteine des norddeutschen Zechsteins.- Zt. dt. geol. Ges., 114, 484-53l.
Fuchtbauer, H. (1968). Carbonate sedimentation and subsidence in the Zechstein Basin
(northern Germany).- in Muller, G. and Friedmann, G.M.(Eds.): Recent Developments in
Carbonate Sedimentology in Central Europe.- Springer, Berlin, 196 - 204.
Harris, M. T. (1989): Modeling carbonate-progradation geometry and sediment -accumulation
rates - a comparison of "MARGIN" results with field data.- in: Franseen, E.K. and Watney,
W.L (Eds.): Sedimentary modeling: Computer simulation of depositional sequences.- Kansas Geol. Survey, Subsurface Geology Series, 12, Lawrence, Kansas, 11-13.
Huttel, P. (1989): Das Stassfurt-Karbonat (Ca2) in Sud-Oldenburg - Fazies und Diagenese
eines Sediments am Nordrand der Hunteschwelle.- Gottinger Arb. Geol. Palaontol., 39, 94 p.
Imbrie, J. and Imbrie, K.P. (1979): Ice ages: Solving the mystery.- McMillan Press, New York,
224p.
Okm
Om
-100 m
-200 m
-300 m
-400m
10 km
20 km
Werra Anhydrite
(A1 )
Fig.27 Ca2 LSW and A2 LST/eTST, East Germany
Acknowledgements
337
PHIL is a trademark of PetroDynamics Inc. (formerly MarcoPolo Software).
BEB Erdgas and Erdal GmbH, Hannover / Germany is thanked for financial and
data support.
Erdoel-Erdgas Gommern GmbH, Gommern / Germany is thanked for providing
data and the permission for publication.
For valuable discussions the authors thank Thomas Aigner, Scott A. Bowman,
Werner Dauben, Chris Kendall, Werner Leu, Eberhard Plein, Ingo Steinhoff and
Walter L. Watney.
We also thank Karen M. Love for her review of this paper.
We gratefully acknowledge the management of BEB Erdgas and Erdoel GmbH,
as well as the W.E.G. publication committee, for permission to publish this paper.
References
Below,A. (1992): Fazies- und geochemische Diagenesestudie im Zechstein 2-Karbonat (Ca2)
Nordwestdeutschlands.- Rep. Geol. Pal. Inst. Univ. Kie1, 60, 147 p.
Fuchtbauer, H. (1964): Fazies, Porositat und Gasinhalt der Karbonatgesteine des norddeutschen Zechsteins.- Zt. dt. geol. Ges., 114, 484-53l.
Fuchtbauer, H. (1968). Carbonate sedimentation and subsidence in the Zechstein Basin
(northern Germany).- in Muller, G. and Friedmann, G.M.(Eds.): Recent Developments in
Carbonate Sedimentology in Central Europe.- Springer, Berlin, 196 - 204.
Harris, M. T. (1989): Modeling carbonate-progradation geometry and sediment -accumulation
rates - a comparison of "MARGIN" results with field data.- in: Franseen, E.K. and Watney,
W.L (Eds.): Sedimentary modeling: Computer simulation of depositional sequences.- Kansas Geol. Survey, Subsurface Geology Series, 12, Lawrence, Kansas, 11-13.
Huttel, P. (1989): Das Stassfurt-Karbonat (Ca2) in Sud-Oldenburg - Fazies und Diagenese
eines Sediments am Nordrand der Hunteschwelle.- Gottinger Arb. Geol. Palaontol., 39, 94 p.
Imbrie, J. and Imbrie, K.P. (1979): Ice ages: Solving the mystery.- McMillan Press, New York,
224p.