Hostname: page-component-586b7cd67f-dsjbd Total loading time: 0 Render date: 2024-11-22T16:16:57.273Z Has data issue: false hasContentIssue false
  • English
  • Français

Tertiary sedimentary development of the Broad Fourteens area, the Netherlands

Published online by Cambridge University Press:  01 April 2016

Th.E. Wong ,
N. Parker  and
P. Horst
Th.E. Wong*
Affiliation:
Netherlands Institute of Applied Geoscience - TNO, PO Box 80015, 3508 TA Utrecht, the Netherlands
N. Parker
Affiliation:
Netherlands Institute of Applied Geoscience - TNO, PO Box 80015, 3508 TA Utrecht, the Netherlands
P. Horst
Affiliation:
Amsterdamse straatweg 312bis, 3551 CT Utrecht, the Netherlands
*
1Corresponding author; e-mail: [email protected]
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

The Broad Fourteens Basin is a NW-SE trending Mesozoic structural element that was affected by inversion movements during the Late Cretaceous (Subhercynian Phase) and Early Tertiary (Laramide Phase). Since the overlying Tertiary section of this area is relatively little studied, a multi-disciplinary investigation was initiated using both seismic and well data. The present study is the first phase of that project and deals exclusively with the stratigraphical framework and sedimentary development based on well logs from approximately forty wells.

The Tertiary sedimentary section in this area (maximum thickness up to approximately 800 m) consists of siliciclastic rocks that generally correlate well with the established lithostratigraphical framework of the Netherlands. However, the highly variable thickness of these lithological units, illustrated by isopach maps for all units, reflect the intricate pattern of sea level movements, differential vertical movements and the ensuing erosion, that took place in this tectonically active area.

Well P06-02, one of the most complete sections in the center of the area, was selected for detailed biostratigraphical analysis to support further stratigraphical subdivision and correlation. This yielded information on both the distribution pattern of various lithological units and the influence of large, partly global, events during basin development. It is concluded that application of detailed sequence stratigraphy in the study area is very problematic and only 2nd and some 3rd order cycles could be recognized.

Keywords

Broad Fourteens BasinstratigraphyTertiarythe Netherlands
Type
Conference papers
Information
Netherlands Journal of Geosciences , Volume 80 , Issue 1 , April 2001 , pp. 85 - 94
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2001

References

Dronkers, A.J. & Mrozek, F.J., 1991. Inverted basins of the Netherlands. First Break 9: 409–425.Google Scholar
Haq, B.U., Hardenbol, J. & Vail, P.R. 1988. Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change. In: Wilgus, C.K., Hastings, B.C., Kendall, C.G.S.C. Posamentier, H.W., Ross, C.A. & Van Wagoner, J.C. (eds): Sea-level changes - An integrated approach. Society of Economic Paleontologists and Mineralogists. Spec. Pubi. 42: 71–108.Google Scholar
Harding, T.P., 1983. Graben hydrocarbon plays and structural styles. Geologie en Mijnbouw 62: 3–23.Google Scholar
Heybroek, P., 1974. Explanation to tectonic maps of the Netherlands. Geologie en Mijnbouw 53: 43–50.Google Scholar
Huyghe, P. & Mugnier, J.-L., 1994. Intra-plate stresses and basin inversion: A case history from the Southern North Sea. In: Roure, F. (ed.) Peri-Tethian Platforms, Edition Technique, Paris: 211–226.Google Scholar
Jacobs, P., 1995a. Eocene sediment supply in Western Belgium as determined through heavy mineral distribution. Contributions to Tertiary and Quaternary Geology 32: 32–52.Google Scholar
Jacobs, P., 1995b. Eocene to early Oligocene deltas in the Southern North Sea Bight, Belgium. In: Oti, M. & Postma, G. (eds): Geology of Deltas. Balkema, Rotterdam: 139–152.Google Scholar
Jacobs, P. & De Batist, M., 1996. Sequence stratigraphy and architecture on a ramp-type continental shelf: the Belgian Palaeogene. Geological Society Special Publications 117: 23–48.Google Scholar
Jacqué, M. & Thouvenin, J., 1975. Lower Tertiary tuffs and volcanic activity in the North Sea. In: Woodland, A.W. (ed.): Petroleum and the continental shelf of Northwest Europe, I Geology. Applied Science Pubi., Barking: 455–465.Google Scholar
Letsch, W.J. & Sissingh, W. 1983. Tertiary stratigraphy of the Netherlands. Geologie en Mijnbouw 62: 305–318.Google Scholar
Morton, A.C. & Knox, R.W.O.B., 1990. Geochemistry of late Paleocene and early Eocene tephras from the North Sea Basin. Journal of the Geological Society 147: 425–437.Google Scholar
Nalpas, T., Le Douaran, S., Brun, J.P., Unternehr, P. & Richard, J.P. 1995. Inversion of the Broad Fourteens Basin (offshore Netherlands), a small-scale model investigation. Sedimentary Geology 95: 237–250.CrossRefGoogle Scholar
Roelofsen, J.W. & de Boer, W.D., 1991. Geology of the Lower Cretaceous Q/l oilfields, Broad Fourteens basin, the Netherlands. In: Spencer, A.M. (ed.): Generation, accumulation, and production of Europe’s hydrocarbons. Special Publication European Association of Petroleum Geoscientists 1, Oxford Univ. Press: 203–216 Google Scholar
Steurbaut, E., 1998. High-resolution holostratigraphy of Middle Paleocene to Early Eocene strata in Belgium and adjacent areas. Palaeontographica Abt. A 247: 91–156.Google Scholar
Van Adrichem Boogaert, A. & Kouwe, W. (eds), 1997. Stratigraphie nomenclature of the Netherlands, revision and update by RGD and NOGEPA. Mededelingen Rijks Geologische Dienst 50, Section I: 1–39.Google Scholar
Van Wagoner, J.C., Mitchum, R.M., Posamentier, H.W. & Vail, P.R., 1987. Seismic stratigraphy interpretation using sequence stratigraphy, part II: Key definitions of sequence stratigraphy. In: Bally, A.W. (ed.): Atlas of Seismic Stratigraphy. American Association of Petroleum Geologists Studies in Geology 27: 1 - 10.Google Scholar
Van Wijhe, D.H., 1987a. The structural evolution of the Broad Fourteens Basin. In: Brooks, J. & Glennie, K.W. (eds): Petroleum geology of North-West Europe, Proc. of the 3rd Conference, London, 1986, Graham & Trotman: 315–323.Google Scholar
Van Wijhe, D.H., 1987b. Structural evolution of inverted basins in the Dutch Offshore. Tectonophysics 137: 171–219.Google Scholar
Vinken, R. (comp.), 1988. The Northwest European Tertiary Basin. Geologisches Jahrbuch A, 100: 508 pp.Google Scholar
Zagwijn, W.H., 1989. The Netherlands during theTertiary and the Quaternary: a case history of coastal lowland evolution. Geologie en Mijnbouw 68: 107–120.Google Scholar
Ziegler, P.A., 1978. Northwestern Europe: tectonics and basin development. Geologie en Mijnbouw 57: 589–626.Google Scholar
Ziegler, P.A., 1990. Geological Atlas of western and Central Europe (2nd. ed.). Shell Int. Petrol. Mij.: 239 pp, 56 enei.Google Scholar