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New stratigraphic insights in the ’Late Jurassic’ of the Southern Central North Sea Graben and Terschelling Basin (Dutch Offshore) and related exploration potential

Published online by Cambridge University Press:  01 April 2016

O.A. Abbink ,
H.F. Mijnlieff ,
D.K. Munsterman  and
R.M.C.H. Verreussel
O.A. Abbink*
Affiliation:
TNO B&O, Geological Survey of the Netherlands, P.O. Box 80015, NL-3508 TA Utrecht, the Netherlands
H.F. Mijnlieff
Affiliation:
TNO B&O, Geological Survey of the Netherlands, P.O. Box 80015, NL-3508 TA Utrecht, the Netherlands
D.K. Munsterman
Affiliation:
TNO B&O, Geological Survey of the Netherlands, P.O. Box 80015, NL-3508 TA Utrecht, the Netherlands
R.M.C.H. Verreussel
Affiliation:
TNO B&O, Geological Survey of the Netherlands, P.O. Box 80015, NL-3508 TA Utrecht, the Netherlands
*
*Corresponding author. Email:oscar.abbink@tno.nl
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Abstract

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Middle Jurassic - Early Cretaceous strata are a target for oil and gas exploration in the Dutch offshore. During the initial stages of the ‘Late Jurassic’ offshore exploration, various oil fields and a few gas fields were discovered of which only one, the F3-FB field, proved to be economically viable. In the Northern Offshore of the Netherlands, latest Middle Jurassic (Callovian) - earliest Cretaceous (Ryazanian) strata are mostly limited to the Dutch Central Graben and Terschelling basins. Outside the Dutch Central Graben and the Terschelling Basin only thin veneers of these strata occur on the fringing highs such as the Schill Grund High and the Step Graben. The geology of this non-marine to shallow marine succession is complex. The combination of lateral facies changes, repetitive log and facies characteristics in time, sea-level and climate changes, salt tectonics and structural compartmentalisation hamper straightforward seismic interpretation and log correlation. The large number of lithostratigraphic units defined in the Stratigraphic Nomenclature of the Netherlands illustrates the complexity of this time-interval.

In recent years, new biostratigraphic techniques and newly acquired stratigraphic data led to the identification of a series of events which can be related to the tectonic, climatic, environmental and stratigraphic development of the ‘Late Jurassic’ in the Dutch Central Graben and Terschelling basins. Based on these data, three stratigraphic sequences can be recognized. Sequence 1 (Callovian - earliest Kimmeridgian) records the initiation of the Dutch Central Graben, Sequence 2 (early Kimmeridgian - early Portlandian) that of the initiation of the Terschelling Basin. During sequence 3 (late Portlandian - Ryazanian) the Dutch offshore was draped by a regional transgression. These insights have directly impact on the exploration potential, which is discussed in two play concepts. The first is a strat-trap play in the fluvial/paralic sediments of Sequence 1 in the lows between the graben boundary and salt domes. The second example is the Spiculite play, which comprises a bioclastic sandstone reservoir at the top of a dome with a 4-way dip closure. These two examples highlight the necessity of understanding the paleoenvironment and geography for assessing the future exploration potential.

Keywords

Dutch offshoreLate Jurassicstratigraphyparalic & shallow marine depositsstratigraphic trapspiculitehydrocarbonsexploration
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 85 , Issue 3 , September 2006 , pp. 221 - 238
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2006

References

Abbink, O.A., 1998. Palynological investigations in the Jurassic of the North Sea region. LPP Contribution Series 8: 192 pp.Google Scholar
Abbink, O.A., Targarona, J., Brinkhuis, H. & Visscher, H., 2001. Late Jurassic to earliest Cretaceous palaeoclimatic evolution of the Southern North Sea. Global and Planetary Change 30: 231–256.CrossRefGoogle Scholar
Abbink, O.A., Van Konijnenburg - Van Cittert, J.H.A. & Visscher, H., 2004a. A Sporomorph Ecogroup Model for the Northwest European Jurassic - Lower Cretaceous I: concepts and framework. Netherlands Journal of Geosciences 83: 17–28.Google Scholar
Abbink, O.A., Van Konijnenburg-Van Cittert, J.H.A., Van der Zwan, C.J. & Visscher, H., 2004b. A Sporomorph Ecogroup Model for the Northwest European Jurassic - Lower Cretaceous II: application to an exploration well from the Dutch North Sea. Netherlands Journal of Geosciences 83: 79–90.Google Scholar
DeGraciansky, P.-C., Hardenbol, J., Jacquin, T., Vail, P.R. & Farley, M.B., 1999. Jurassic sequence chronostratigraphy/biochronostratigraphy. In: De, Graciansky et al. (eds): Mesozoic-Cenozoic Sequence Stratigraphy of European Basins. Special Publication of the Society of Economists, Paleontologists and Mineralists, 60: Charts 6 and 7.CrossRefGoogle Scholar
Duxbury, S., Kadolsky, D. & Johansen, S., 1999. Sequence stratigraphic subdivision of the Humber Group in the Outer Moray Firth (UKCS, North Sea). In: Jones, R.W. & Simmons, M.D. (eds): Biostratigraphy in Production and Development Geology. Geological Society London, Special Publications 152: 23–54.Google Scholar
Gammon, P.R. & James, N.P., 2001. Palaeogeographical influence on late Eocene biosiliceous sponge-rich sedimentation, southern Western Australia. Sedimentology 48: 559–584.CrossRefGoogle Scholar
Gammon, P.R., James, N.P. & Pisera, A., 2000. Eocene spiculites and spongolites in south-western Australia: Not deep, not polar, but shallow and warm. Geology 28: 855–858.2.0.CO;2>CrossRefGoogle Scholar
Gradstein, F., Ogg, J. & Smith, A., 2004. A Geologic Time Scale 2004. Cambridge University Press (Cambridge): 589 pp.Google Scholar
Haq, B.U., Hardenbol, J., & Vail, P.R., 1988. Mesozoic & Cenozoic chronostratigraphy and cycles of sea level change. In: Wilgus, C. K., Hastings, B. S. et al. (eds): Sea Level Changes; An Integrated Approach. Special Publication of the Society of Economists, Paleontologists and Mineralists 42: 71–108.Google Scholar
Herngreen, G.F.W. & Wong, Th.E., 1989. Revision of the ’Late Jurassic’ stratigraphy of the Dutch Central North Sea Graben. Geologie & Mijnbouw 68: 73–105.Google Scholar
Herngreen, G.F.W., Kerstholt, S.J. & Munsterman, D.K., 2000. Callovian-Ryazanian (’Upper Jurassic’) palynostratigraphy of the Central North Sea Graben and Vlieland Basin, the Netherlands. Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO 63: 1–99.Google Scholar
Jacquin, T., Dardeau, G., Durlet, C., DeGraciansky, P.-C. & Hantzpergue, P., 1999. The North Sea cycle: an overview of 2nd order Transgressive/ Regressive facies cycles in Western Europe. In: De, Graciansky et al. (eds): Mesozoic-Cenozoic Sequence Stratigraphy of European Basins. Special Publication of the Society of Economists, Paleontologists and Mineralists 60: 445–466.Google Scholar
Kiessling, W., Flügel, E. & Golonka, J., 1999. Paleoreef maps: evaluation of a comprehensive database on Phanerozoic reefs. American Association of Petroleum Geologists Bulletin 83: 1552–1587.Google Scholar
Leinfelder, R.R., Werner, W., Nose, M., Schmid, D.U. Krautter, M., Laternser, R. Takacs, M & Hartmann, D., 1996. Paleoecology, growth Parameters and Dynamics of coral, Sponge and Microbilite Reefs from the Late Jurassic. In: Reitner, J., Neuweiler, F. & Gunkel, F. (eds): Global and Regional Controls on Biogenic Sedimentation. I Reef Evolution. Research reports - Göttinger Arbeiten zur Geologie und Paläontologie, Sonderband: 227–248.Google Scholar
Lokhorst, A. (ed.), 1998. Northwest European Gas Atlas - composition and isotope ratios of natural gases. Netherlands Institute of Applied Geoscience TNO report, Haarlem, the Netherlands. ISBN 90-72869-60-5.Google Scholar
Mijnlieff, H.F., 2001. Top Pre-Permian distribution map & some thematic regional geologic maps of the Netherlands. ICCP conference August 2003, Utrecht, the Netherlands: poster presentation.Google Scholar
Odin, G.S. & Matter, A., 1981. De Glauconarium Origine. Sedimentology 28: 611–641.Google Scholar
Partington, M.A.P., Copestake, P., Mitchener, B.C. & Underhill, J.R., 1993. Biostratigraphic correlation of genetic stratigraphic sequences in the Jurassic - lowermost Cretaceous (Hettangian - Ryazanian) of the North Sea and adjacent areas. In: Parker, J.R., (ed.): Petroleum Geology of Northwest Europe: Proceedings of the 4th Conference: 371–386.Google Scholar
Partington, M.A.P., Mitchener, B.C., Milton, N.J. & Fraser, A.J., 1993a. Genetic sequence stratigraphy for the North Sea Late Jurassic and Early Cretaceous of the North Sea: distribution and prediction of Kimmeridgian-Late Ryazanian reservoirs in the North Sea and adjacent areas. In: Parker, J.R. (ed.): Petroleum Geology of Northwest Europe, Proceedings of the 4th Conference: 347–370.Google Scholar
Riding, J.B. & Thomas, J.E., 1992. Dinoflagellate cysts of the Jurassic System. In: Powell, A.J. (ed.): A Stratigraphic Index of Dinoflagellate Cysts: 7–98.Google Scholar
Rioult, M, Dugué, O., Jan du Chêne, R., Ponsot, C., Fily, G., Moron, J. & Vail, P.R., 1991. Outcrop Sequence stratigraphy of the Anglo-Paris basin Middle to Upper Jurassic (Normandy, Maine, Dorset). Bulletin des Centres de Recherches Exploration-Production Elf-Aquitaine 15: 101–194.Google Scholar
Underhill, J.R. & Partington, M.A.P., 1993. Jurassic thermal doming and deflation in the North Sea: implications of sequence stratigraphic evidence. In: Parker, J.R. (ed.): Petroleum Geology of Northwest Europe: Proceedings of the 4th Conference: 337–345.Google Scholar
Vail, P.R., Audemard, F., Bowman, S.A., Eisner, P.N. & Perez-Cruz, C., 1991. The stratigraphic signatures of tectonics eustacy and sedimentology - an overview. In: Einsele, G. et al. (eds): Cycles and events in stratigraphy: 250–275.Google Scholar
Van Adrichem Boogaert, H.A. & Kouwe, W.L.F.P., 1993. Stratigraphic nomenclature of the Netherlands, revision and update by RGD and NOGEPA. Mededelingen Rijks Geologische Dienst Nieuwe Serie 50.Google Scholar
Werver, O., 1996. Ichnofauna in relation to the depositional environment of Jurassic and Cretaceous sediments in the Netherlands. Part I: Atlas of Ichnofauna. Stichting Educatie Centrum Ammonietenhoeve. ISBN 90-803304-1-8.Google Scholar
Werver, O., 1997. Ichnofauna and flora in relation to their environment of sediments in the Central Graben, Netherlands Offshore. Environmental interpretation based on trace fossils from the Upper Jurassic - Lower Cretaceous. Stichting Educatie Centrum Ammonietenhoeve. ISBN 90-803304-1-8.Google Scholar
Ziegler, P.A., 1990. Geological Atlas of Western and Central Europe, 2nd and completely revised edition, Shell International Exploration and Production B. V., the Hague, Geological Society Publishing House (Bath): 239 pp.Google Scholar