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3D reconstruction of salt movements within the deepest post-Permian structure of the Central European Basin System - the Glueckstadt Graben

Published online by Cambridge University Press:  01 April 2016

Y. Maystrenko ,
U. Bayer  and
M. Scheck-Wenderoth
Y. Maystrenko*
Affiliation:
GeoForschungsZentrum Potsdam, Section 4.3, Telegrafenberg, 14473 Potsdam, Germany
U. Bayer
Affiliation:
GeoForschungsZentrum Potsdam, Section 4.3, Telegrafenberg, 14473 Potsdam, Germany
M. Scheck-Wenderoth
Affiliation:
GeoForschungsZentrum Potsdam, Section 4.3, Telegrafenberg, 14473 Potsdam, Germany
*
*Corresponding author. Email:yuram@gfz-potsdam.de
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Abstract

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The Glueckstadt Graben is a prominent structure of the Central European Basin System, where the sedimentary patterns are extensively affected by Permian salt movements. The relations of the sedimentary patterns to salt structures have been analyzed through present-day distributions of sediments. In addition, a three-dimensional backward modelling approach has been applied to determine the original salt distribution in response to the unloading due to sequential backstripping of the stratigraphic layers. The results of the modelling reveal the thickness distribution of the Permian salt for 5 time intervals from the end of the Triassic to present day. Spatial agreement has been found between the development of the depleted zone of the Permian salt through time and the observed distribution of the maximum subsidence for the different stratigraphic units above the salt. The sedimentation centres for each time interval are always located above the zone of reduced or depleted Permian salt. In the central part of the Glueckstadt Graben, the depletion occurred already in the Triassic and perfectly correlates with the thickest Triassic. During the Jurassic, Cretaceous and Tertiary, the areas of depleted Permian salt shifted towards the basin flanks, and the same occurred with the centres of maximum sediment deposition. Thus, the results of the modelling strongly support the conclusion that salt withdrawal has played a major role during the Meso-Cenozoic evolution of the Glueckstadt Graben and that the progressive depletion of the Permian salt layer, from the central part towards the margins, created the large part of the accommodation space for sedimentation in addition to tectonic subsidence.

Furthermore, our study has several important implications for salt behaviour in different tectonic settings. In general, the results of modelling indicate a good correlation between the main phases of salt movements and tectonic events in the area under consideration. During the Triassic, the first stage of diapirism in the Glueckstadt Graben occurred within the central part of the basin. Regional extension may have triggered reactive diapirism and caused the formation of the deep primary rim synclines. Once the salt structures had reached the critical size, buoyancy forces supported their continued growth until the Jurassic when extension-induced regional stresses once more affected the Glueckstadt Graben. The results of the modelling indicate very little salt activity during the late Early Cretaceous-early Late Cretaceous when the area of the Glueckstadt Graben was tectonically silent. Therefore, our study supports the concept of tectonically induced salt movements which can be interrupted during the absence of tectonic forces. Salt movements were reactivated in the marginal troughs by compressional forces during the latest Late Cretaceous-Early Cenozoic. Paleogene-Neogene salt withdrawal led to the growth of N-S oriented salt structures mainly at the margins of the basin. This phase of salt tectonics correlates temporally with almost W-E extension. This indicates a renewed change in tectonic regime after Late Cretaceous-Early Cenozoic compression.

Keywords

Triassic grabensalt tectonics3D modellingNW Germany
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 85 , Issue 3 , September 2006 , pp. 181 - 196
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2006

References

Baldschuhn, R., Binot, F., Fleig, S. & Kockel, F. (eds), 2001. Geotektonischer Atlas von Nordwest-Deutschland und dem deutschen Nordsee-Sektor - Strukturen, Struckurenwicklung, Paläogeographie. Geologisches Jahrbuch A 153: 1–88, 3 CD-Rs.Google Scholar
Baldschuhn, R., Frisch, U. & Kockel, F. (eds), 1996. Geotektonischer Atlas von NW-Deutschland 1 : 300,000. 4 pp., 65 maps, Bundesanstalt für geowissen-schaften und Rohstoffe, Hannover.Google Scholar
Bayer, U., Scheck, M., Rabbel, W., Krawczyk, C.M., Götze, H.-J., Stiller, M. Beilecke, Th., Marotta, A.M., Barrio-Alvers, L. & Kuder, J., 1999. An integrated study of the NE German Basin. Tectonophysics 314: 285–307.Google Scholar
Best, G., Kockel, F., Schoeneich, H., 1983. Geological history of the southern Horn graben. Geologie en Mijnbouw 62: 25–33.Google Scholar
Betz, D., Führer, F. & Plein, E., 1987. Evolution of the lower Saxony basin. Tectonophysics 137: 127–170.CrossRefGoogle Scholar
Boigk, H., 1981. Erdöl und Erdölgas in der Bundesrepublik Deutschland: Erdölprovinzen, , Felder, , Förderung, , Vorräte, , Lagerstättentechnik, . Germany, Stuttgart, Enke: 330 pp.Google Scholar
Brink, H.J., Dürschner, H. & Trappe, H., 1992. Some aspects of the late and post-Variscan development of the Northwestern German Basin. Tectonophysics 207: 65–95.Google Scholar
Brink, H.J., Franke, D., Hoffmann, N., Horst, W. & Oncken, O., 1990. Structure and evolution of the North German Basin. In: Freeman, R., Giese, P. & Mueler, St. (eds): The European Geotraverse: Integrative Studies. European Science Foundation (Strasbourg): 195–212.Google Scholar
Britze, P. & Japsen, P., 1991. The Danish Basin. Triassic. Isochore map: Danmarks Geologiske Undersogelse (DGU) Miloeministeriet, Copenhagen, DGU map series no. 31, 1 sheet, scale 1 : 400,000.Google Scholar
Clausen, O.R. & Pedersen, P.K., 1999. The Triassic structural evolution of the southern margin of the Ringkøbing-Fyn-High, Denmark. Marine and Petroleum Geology 16: 653–665.Google Scholar
Dadlez, R., 2003. Mesozoic thickness pattern in the Mid-Polish Trough. Geological Quarterly 47 (3): 223–240.Google Scholar
Daudre, B. & Cloetingh, S., 1994. Numerical modelling of salt diapirism: influence of the tectonic regime. Tectonophysics 240: 59–79.CrossRefGoogle Scholar
Erratt, D., Thomas, G.M. & Wall, G.R.T., 1999. The evolution of the Central North Sea Rift. In: Fleet, A.J. & Boldy, S.A.R., (eds): Petroleum geology of Northwest Europe; proceedings of the 5th conference. The Geological Society of London, London, United Kingdom: 63–82.Google Scholar
Evans, D., Graham, C., Armour, A. & Bathurst, P., 2003. The Millennium Atlas: Petroleum geology of the central and northern North Sea. The Geological Society of London (London): 990 pp.Google Scholar
Garetsky, R.G., Ludwig, A.O., Schwab, G. & Stackebrandt, W. (eds), 2001. Neogeodynamics of the Baltic Sea depression and adjacent areas. Brandenburgische Geowissenschaftliche Beiträge 1-2001: 47 pp, 8 maps.Google Scholar
Guglielmo, G.J., Vendeville, B.C. & Jackson, M.P.A., 1999. Isochores and 3-D visualization of rising and falling salt diapirs. Marine and Petroleum Geology 16: 849–861.Google Scholar
Ismail-Zadeh, A., Tsepelev, I., Talbot, C. & Korotkii, A., 2004. Three-dimensional forward and backward modelling of diapirism: numerical approach and its applicability to the evolution of salt structures in the Pricaspian basin. Tectonophysics 387: 81–103.Google Scholar
Jaritz, W., 1969. Epiorogenese in Nordwestdeutschland im hoheren Jura und in der Unterkreide. Geologische Rundschau 59, 1 Taf.: 114–124.Google Scholar
Jaritz, W. 1980. Einige Aspekte der Entwicklungsgeschichte der nordwest-deutschen Salzstöcke. Zeitschrift der Deutschen Geologischen Gesellschaft 131, 8 Abb: 387–408.Google Scholar
Jordan, H. & Kockel, F., 1991. Die Leinetal-Structur und ihr Umfeld - ein tektonisches Konzept fur Südniedersachsen. Geologisches Jahrbuch A 126: 171–196.Google Scholar
Jordt, H., Faleide, J.I., Bjerlykke, K. & Ibrahim, M.T., 1995. Cenozoic sequence stratigraphy of the central and northern North Sea Basin: tectonic development, sediment distribution and provenance areas. Marine and Petroleum Geology 12: 845–879.Google Scholar
Kaus, B.J.P. & Podladchikov, Y.Y., 2001. Forward and reverse modeling of the three-dimensional viscous Rayleigh-Taylor instability. Geophysical Research Letters 28: 1095–1098.Google Scholar
Kockel, F., 2002. Rifting processes in NW-Germany and the German North Sea Sector. Geologie en Mijnbouw 81: 149–158.Google Scholar
Kockel, F., 2003. Problems of diapirism in northern Germany. Geologos 6: 57–88.Google Scholar
Koyi, H., 1998. The shaping of salt diapirs. Journal of Structural Geology 20: 321–338.Google Scholar
Koyi, H., Jenyon, M.K. & Petersen, K., 1993. The effects of basement faulting on diapirism. Journal of Petroleum Geology 16 (3): 285–312.Google Scholar
Krzywiec, P., 2004. Triassic evolution of the Klodawa salt structure: basement-controlled salt tectonics within the Mid-Polish Trough (Central Poland). Geological Quarterly 48: 123–134.Google Scholar
Lamarche, J. & Scheck-Wenderoth, M., 2005. 3D structural model of the Polish Basin. Tectonophysics 397: 73–91.Google Scholar
Lehne, R. & Sirocko, F., 2005. Quantification of recent movement potentials in Schleswig-Holstein (Germany) by GIS-based calculation of correlation coefficients. International Journal of Earth Sciences 94: 1094–1102.Google Scholar
Lokhorst, A. (ed.), 1998. The Northwest European gasatlas. Netherlands Institute of Applied Geoscience TNO (Haarlem); ISBN 90-72869-60-5.Google Scholar
Maystrenko, Y., Bayer, U. & Scheck-Wenderoth, M., 2005a. The Glueckstadt Graben, a sedimentary record between the North and Baltic Sea in north Central Europe. Tectonophysics 397: 113–126.Google Scholar
Maystrenko, Y., Bayer, U. & Scheck-Wenderoth, M., 2005b. Structure and evolution of the Glueckstadt Graben due to salt movements. International Journal of Earth Sciences 94: 799–814.CrossRefGoogle Scholar
Mazur, S. & Scheck-Wenderoth, M., 2005. Constraints on the tectonic evolution of the Central European Basin System revealed by seismic reflection profiles from Northern Germany. Netherlands Journal of Geosciences / Geologie en Mijnbouw 84: 389–401.Google Scholar
Mazur, S., Scheck-Wenderoth, M. & Krzywiec, P., 2005. Different modes of the Late Cretaceous - Early Tertiary inversion in the North German and Polish basins. International Journal of Earth Sciences 94: 782–798.Google Scholar
Moeller, J.J. & Rasmussen, E.S., 2003. Middle Jurassic - Early Cretaceous rifting of the Danish Central Graben. In: Ineson, J.R. & Surlyk, F. (eds): The Jurassic of Denmark and Greenland. Geological Survey of Denmark and Greenland, Copenhagen: 247–264.Google Scholar
Nielsen, S.B., 2002. A post mid-Cretaceous North Sea model. Bulletin of the Geological Society of Denmark 49: 187–204.Google Scholar
NITG, 2004. Geological Atlas of the Netherlands - onshore (1 : 1,000,000). Netherlands Institute for Applied Geoscience TNO - National Geological Survey (Utrecht): 103 pp.Google Scholar
Oakman, C.D. & Partington, M.A., 1998. Cretaceous. In: Glennie, K.W., (ed.) Petroleum geology of the North Sea, basic concepts and recent advances (4th edition). Blackwell Scientific Publications, Oxford: 294–349.Google Scholar
Otto, V., 2003. Inversion-related features along the southeastern margin of the North German Basin (Elbe Fault System). Tectonophysics 373: 107–123.Google Scholar
Pharaoh, T.C., 1999. Palaeozoic terranes and their lithosphere boundaries within the Trans-European Suture Zone (TESZ): a review. Tectonophysics 314: 17–41.Google Scholar
Poliakov, A.N.B., van Balen, R., Podladchikov, Yu., Daudré, B., Cloetingh, S. & Talbot, C., 1993. Numerical analysis of how sedimentation and redistribution of surficial sediments affects salt diapirism. Tectonophysics 226: 199–216.Google Scholar
Rodon, S. & Littke, R., 2005. Thermal maturity in the Central European Basin system (Schleswig-Holstein area): results of ID basin modelling and new maturity maps. International Journal of Earth Sciences 94: 815–833.Google Scholar
Roemer, M.-M. & Neugebauer, H.J., 1991. The salt dome problem: a multilayered approach. Journal of Geophysical Research 96: 2389–2396.Google Scholar
Sannemann, D., 1968. Salt-stock families in northwestern Germany. In: Braunstein, J. & O’Brien, G. (eds): Diapirism and diapirs. AAPG publication: 261–270.Google Scholar
Scheck, M. & Bayer, U., 1999. Evolution of the Northeast German Basin - inferences from 3D structural modelling and subsidence analysis. Tectonophysics 313: 145–169.Google Scholar
Scheck, M., Bayer, U. & Lewerenz, B., 2003a. Salt movements in the Northeast German Basin and its relation to major post-Permian tectonic phases - results from 3D structural modelling, backstripping and reflection seismic data. Tectonophysics 361: 277–299.Google Scholar
Scheck, M., Bayer, U. & Lewerenz, B., 2003b. Salt redistribution during extension and inversion inferred from 3D backstripping. Tectonophysics 373: 55–73.Google Scholar
Scheck, M., Bayer, U., Otto, V., Lamarche, J., Banka, D. & Pharaoh, T., 2002. The Elbe Fault System in North central Europe - a basement controlled zone of crustal weakness. Tectonophysics 360: 281–299.Google Scholar
Scheck-Wenderoth, M. & Lamarche, J., 2005. Crustal memory and basin evolution in the Central European Basin System - new insights from a 3D structural model. Tectonophysics 397: 143–165.Google Scholar
Schmeling, H., 1987. On the relation between initial conditions and late stages of Rayleigh-Taylor instabilities. Tectonophysics 133: 65–80.Google Scholar
Schultz-Ela, D., Jackson, M.P.A. & Vendeville, B., 1993. Mechanics of active salt diapirism. Tectonophysics 228: 275–312.Google Scholar
Sclater, J.G. & Christie, P.A.F., 1980. Continental stretching: an explanation of the post-Mid-Cretaceous subsidence of the central North Sea basin. Journal of Geophysical Research 85-B7: 3711–3739.Google Scholar
Stovba, S.M. & Stephenson, R.A., 2003. Style and timing of salt tectonics in the Dniepr-Donets Basin (Ukraine): implications for triggering and driving mechanisms of salt movement in sedimentary basins. Marine and Petroleum Geology 19: 1169–1189 Google Scholar
Trusheim, F., 1960. Mechanism of salt migration in North Germany. AAPG Bulletin 44: 1519–1540.Google Scholar
Van Hoorn, B., 1987. Structural evolution, timing and tectonic style of the Sole Pit inversion. Tectonophysics 137: 239–284.Google Scholar
Van Wijhe, D.H., 1987. Structural evolution of inverted basins in the Dutch offshore (North Sea). Tectonophysics 137: 171–219.Google Scholar
Vejbaek, O.V., 1990. The Horn Graben, and its relationship to the Oslo Graben and the Danish Basin. Tectonophysics 178: 29–49.Google Scholar
Vejbaek, O.V. & Britze, P., 1994. Top of the pre-Zechstein rocks. Sub- and supercrop map: Danmarks Geologiske Undersogelse (DGU) Miloeministeriet, Copenhagen, DGU map series no. 45, 1 sheet, scale 1 : 750,000.Google Scholar
Vendeville, B.C. & Jackson, M.P.A., 1992. The rise of diapirs during thin-skinned extension. Marine and Petroleum Geology 9: 331–353.Google Scholar
Vendeville, B.C., John, A. & Jackson, K.G., 2002. A New Interpretation of Trusheim’s Classic Model of Salt-Diapir Growth. Gulf Coast Association of Geological Societies Transactions 52: 943–952.Google Scholar
Woidt, W.-D., 1978. Finite element calculations applied to salt dome analysis. Tectonophysics 50: 369–386.Google Scholar
Ziegler, P., 1990. Geological atlas of Western and Central Europe. 2nd ed. Geol. Soc. Publ. House, Bath, Shell International Petroleum Mij. B.v.: 239 pp.Google Scholar
Ziegler, P., 1992. European Cenozoic rift systems. Tectonophysics 208: 91–111.Google Scholar