Cross-border correlations showing diachronous lithostratigraphic units in the southeastern North Sea Basin during the Early Oligocene (middle-late Rupelian)

Keywords: Dinoflagellate cyst analysis, geophysical logs, Boom and Steensel members (NL), Boom and Eigenbilzen formations (B), Oligocene

Abstract

Wireline log correlation panels of palynologically analysed boreholes illustrate lateral facies transitions within Rupelian age strata of the Dutch Rupel Formation across the southeastern North Sea Basin. The middle to upper part of the Rupel Formation consists of clays and silts of the Boom Member and the overlying sandier Steensel Member. In the Mill and Goirle boreholes in the Dutch Province of North Brabant, the Boom Member is thickly developed and represents the middle to upper Rupelian (biozones NSO3 to NSO5a), while the Steensel Member is rather thinly developed and only comprises the uppermost Rupelian (biozone NSO5a). Borehole log correlations show that towards the south (or more proximal to the palaeo-continent) the Rupel Formation becomes sandier and the clayey Boom Member thins in favour of the sandy superjacent Steensel Member. Palynological analyses confirm that the Boom Member is restricted to the middle Rupelian (biozone NSO3) age here, and that the superjacent Steensel Member is of middle to upper Rupelian age (biozones NSO3 to NSO5a). Geological models constructed for northern Belgium propose that this facies transition occurs rather sharply, along a WSW-ENE oriented zone parallel to the presumed shoreline at that time. The results of this study support this interpretation and extend the trend towards the Netherlands.

References

Bujak, J.P. & Mudge, D., 1994. A high resolution North Sea Eocene dinocyst zonation. Journal of the Geological Society of London 151(3): 449–462.CrossRefGoogle Scholar

Deckers, J., De Koninck, R., Bos, S., Broothaers, M., Dirix, K., Hambsch, L., Lagrou, D., Lanckacker, T., Matthijs, J., Rombaut, B., Van Baelen, K. & Van Haren, T. Geologisch (G3Dv3) en hydrogeologisch (H3D) 3D-lagenmodel van Vlaanderen. Studie uitgevoerd in opdracht van het Vlaams Planbureau voor Omgeving, departement Omgeving en de Vlaamse Milieumaatschappij. VITO, Mol, VITO-rapport 2018/RMA/R/1569, 2019. https://archief-algemeen.omgeving.vlaanderen.be/xmlui/handle/acd/251494 Google Scholar

Deckers, J., Vernes, R., Dabekaussen, W., Den Dulk, M., Doornenbal, H., Dusar, M., Matthijs, J., Menkovic, A., Reindersma, R., Walstra, J., Westerhoff, W. & Witmans, N., 2014. Geologisch en hydrogeologisch 3D model van het Cenozoïcum van de Roerdalslenk in Zuidoost-Nederland en Vlaanderen (H3O-Roerdalslenk), VITO-rapport, 2014/ETE/R/1, 200 pp.Google Scholar

De Man, E., Van Simaeys, S., Vandenberghe, N., Harris, W.B. & Wampler, J.M, 2010. On the nature and chronostratigraphic position of the Rupelian and Chattian stratotypes in the southern North Sea basin. International Union of Geological Sciences, Episodes 33(1): 3–14.Google Scholar

Dybkjær, K. & Piasecki, S., 2010. Neogene dinocyst zonation for the eastern North Sea Basin, Denmark. Review of Palaeobotany and Palynology 161(1): 1–29. DOI: 10.1016/j.revpalbo.2010.02.005.CrossRefGoogle Scholar

Fensome, R.A., Williams, G.L. & MacRae, R.A., 2019. Lentin and Williams index of fossil dinoflagellates. AASP Contribution Series 50: 1173 pp.Google Scholar

Halet, F., 1936. Le Néogène et l’Oligocène entre Hasselt et Genk. Bulletin de la Société belge de Géologie, de Paléontologie et d’Hydrologie 46: 194–199.Google Scholar

Heilmann-Clausen, C. & Van Simaeys, S., 2005. Dinoflagellate cysts from the Middle Eocene to ?lowermost Oligocene succession in the Kysing research borehole, central Danish basin. Palynology 29(1): 143–204. DOI: 10.1080/01916122.2005.9989606.CrossRefGoogle Scholar

Köthe, A., 2003. Dinozysten-Zonierung im Tertiär Norddeutschlands. Revue Paleobiologie 22(2): 895–923.Google Scholar

Laenen, B., 1998. The geochemical signature of relative sea-level cycles recognised in the Boom Clay. In: Aardkundige Mededelingen. vol. 9, University Press Leuven: 61–82.Google Scholar

Louwye, S., 2005. The Early and Middle Miocene transgression at the southern border of the North Sea Basin (northern Belgium). Geological Journal 40(4): 441–456. DOI: 10.1002/gj.1021.CrossRefGoogle Scholar

Louwye, S., Deckers, J., Verhaegen, J., Adriaens, J. & Vandenberghe, N., 2020. A review of the lower and middle Miocene of northern Belgium. Geologica Belgica 23(3-4): 137–156. DOI: 10.20341/gb.2020.010.CrossRefGoogle Scholar

Matthijs, J., 1999. Toelichtingen bij de geologische kaart van België, Vlaams Gewest: kaartblad 25, Hasselt [1: 50 000]. In: Belgische Geologische Dienst en Ministerie van de Vlaamse Gemeenschap. Afdeling Natuurlijke Rijkdommen en Energie (Brussel): 104 pp.Google Scholar

Munsterman, D.K. I De resultaten van het palynologisch onderzoek naar de ouderdom en het afzettingsmilieu van boring 58G192 (Herkenbosch), traject: 43.8-260.25 m. TNO rapport NITG 98-224-B 1998. https://www.dinoloket.nl/ondergrondmodellenforlithologicalandlithostratigraphicinterpretation.Google Scholar

Munsterman, D.K., 2022. De resultaten van de palynologische studie naar de ouderdom van boring Mill, B46C0478, interval: 10-481 m (Peelhorst), Rapport TNO 2022 R10095: 22 pp.Google Scholar

Munsterman, D.K. & Brinkhuis, H., 2004. A southern North Sea Miocene dinoflagellate cyst zonation. Netherlands Journal of Geosciences 4(4): 267–285. DOI: 10.1017/S0016774600020369.CrossRefGoogle Scholar

Munsterman, D.K. & Deckers, J., 2020. The Oligocene/Miocene boundary in the ON-Mol-1 and Weelde boreholes along the southern margin of the North Sea Basin, Belgium. Geologica Belgica 23(3-4): 127–135. DOI: 10.20341/gb.2020.007.CrossRefGoogle Scholar

Munsterman, D.K. & Deckers, J., 2022. Biostratigraphic ages and depositional environments of the upper Oligocene to lower Miocene Veldhoven Formation in the central Roer Valley Rift System (SE Netherlands-NE Belgium). Netherlands Journal of Geosciences 101: e6. DOI: 10.1017/njg.2022.3.CrossRefGoogle Scholar

Munsterman, D.K., ten Veen, J.H., Menkovic, A., Deckers, J., Witmans, N., Verhaegen, J., Kerstholt-Boegehold, S.J., van de Ven, T. & Busschers, F.S., 2019. An updated and revised stratigraphic framework for the Miocene and earliest Pliocene strata of the Roer Valley Graben and adjacent blocks. Netherlands Journal of Geosciences 98: e8. DOI: 10.1017/njg.2019.10.CrossRefGoogle Scholar

NAM & RGD, 1980. Stratigraphic Nomenclature of the Netherlands. Verhandelingen KNGMG 32: 77 pp.Google Scholar

Ogg, J.G., Ogg, G. & Gradstein, F.M., 2016. A Concise Geologic Time Scale: 240 pp.Google Scholar

Powell, A.J., 1992. Dinoflagellate cysts of the Tertiary System. In: Powell, A.J., A stratigraphic index of dinoflagellate cysts, 155–272.CrossRefGoogle Scholar

Sliwinska, K.K., 2019. Early Oligocene dinocysts as a tool for paleoenvironment reconstruction and stratigraphic framework-a case study from a North Sea well. Journal of Micropalaeontology 38: 143–176. DOI: 10.5194/jm-38-143-219.CrossRefGoogle Scholar

Stover, L.E. & Hardenbol, J., 1994. Dinoflagellates and depositional sequences in the Lower Oligocene (Rupelian) Boom Clay Formation. Belgium. Bulletin Society Belgium Geology 102(1-2): 5–77.Google Scholar

TNO-GDN, 2023. Stratigrafische Nomenclator van Nederland. TNO – Geologische Dienst Nederland. http://www.dinoloket.nl/stratigrafische-nomenclator.Google Scholar

Van Adrichem Boogaert, A.H. & Kouwe, W.F.P. (eds), 1993-1997. Stratigraphic Nomenclature of the Netherlands, revision and update by RGD and NOGEPA, Mededelingen Rijks Geologische Dienst 50, Section I, 39 pp.Google Scholar

Vandenberghe, N., De Craen, M. & Wouters, L., 2014. The boom clay geology from sedimentation to present-day occurrence. A review. Memoirs of the Geological Survey of Belgium 60: 78–p.Google Scholar

Vandenberghe, N., Hager, H., van den Bosch, M., Verstraelen, A., Leroi, S., Steurbaut, E., Prüfert, J. & Laga, P, 2001. Stratigraphical Correlation by calibrated well logs in the Rupel Group between North Belgium, the Lower-Rhine area in Germany and Southern Limburg and the achterhoek, in The Netherlands, Aardkundige Mededelingen 11. University Press Leuven: 69–84.Google Scholar

Vandenberghe, N., Harris, W., Wampler, J., Houthuys, R., Louwye, S., Adriaens, R., Vos, K., Lanckacker, T., Matthijs, J., Deckers, J., Verhaegen, J., Laga, P., Westerhoff, W. & Munsterman, D., 2014. The implications of K-Ar glauconite dating of the Diest Formation on the paleogeography of the Upper Miocene in Belgium. Geologica Belgica 17: 161–174.Google Scholar

Vandenberghe, N. & Mertens, J., 2013. Differentiating between tectonic and eustasy signals in the Rupelian Boom Clay cycles (Southern North Sea Basin). Newsletters on Stratigraphy 46(3): 319–337.CrossRefGoogle Scholar

Vandenberghe, N. & Wouters, L., 2023. Lithostratigraphic Information Sheets Rupel Group. National Commission for Stratigraphy Belgium, proposal for discussion. 43 pp. https://ncs.naturalsciences.be/sites/default/files/Rupel%20Group%20discussion%2020230718.pdf Google Scholar

Van Simaeys, S., Munsterman, D.K. & Brinkhuis, H., 2004. Oligocene dinoflagellate cyst biostratigraphy of the southern North Sea Basin. Review of Palaeobotany and Palynology 134(1-2): 105–128.CrossRefGoogle Scholar

Vernes, R.W., Deckers, J., Bakker, M.A.J., Bogemans, F., De Ceukelaire, M., Doornenbal, J.C., den Dulk, M., Dusar, M., Van Haren, T.F.M., Heyvaert, V.M.A., Kiden, P., Kruisselbrink, A.F., Lanckacker, T., Menkovic, A., Meyvis, B., Munsterman, D.K., Reindersma, R., ten Veen, J.H., van de Ven, T.J.M., Walstra, J. & Witmans, N., 2018. Geologisch en hydrogeologisch 3D model van het Cenozoïcum van de Belgisch-Nederlandse grensstreek van Midden-Brabant / De Kempen (H3O – De Kempen). Studie uitgevoerd door VITO, TNO-Geologische Dienst Nederland en de Belgische Geologische Dienst in opdracht van Vlaams Planbureau voor Omgeving, Vlaamse Milieumaatschappij, TNO, Geologische Dienst Nederland, Nederlandse Provincie Noord-Brabant, Brabant Water, Programmabureau KRW/DHZ Maasregio.Google Scholar

Vernes, R.W., Deckers, J., Walstra, J., Kruisselbrink, A.F., Menkovic, A., Bogemans, F., De Ceukelaire, M., Dirix, K., Dusar, M., Hummelman, H.J., Maes, R., Meyvis, B., Munsterman, D.K., Reindersma, R., Rombaut, B., Van Baelen, K., Van de Ven, T.J.M., Van Haren, T. & Welkenhuysen, K., 2023. Geologisch en hydrogeologisch 3D model van het Cenozoïcum van de Belgisch-Nederlandse grensstreek van De Noorderkempen/West-Brabant (H3O-De Voorkempen), TNO-rapport 2023 R10347, VITO-rapport 2023/RMA/R/2906, BGD-rapport 2023/02, 156 pp.Google Scholar

Vis, G.J., Verweij, J.M. & Koenen, M., 2016. The Rupel Clay Member in the Netherlands; towards a better understanding of its depositional environment. Netherlands Journal of Geosciences 95(3): 221–251. DOI: 10.1017/njg.2016.25.
Published
2024-05-13
How to Cite
Munsterman , D. K., & Deckers , J. (2024). Cross-border correlations showing diachronous lithostratigraphic units in the southeastern North Sea Basin during the Early Oligocene (middle-late Rupelian). Netherlands Journal of Geosciences, 103. https://doi.org/10.1017/njg.2024.10
Section
Regular paper