Depositional environment of the Oligocene Rupel Clay in well Grashoek-l, Peel region, The Netherlands.
Abstract
A continuously cored marine Oligocene Rupel Clay of the N.A.M. well Grashoek-1 (Peel region, the Netherlands) yielded a benthonic foraminiferal fauna indicative of a bathyal environment with a seadepth below 300-500 m.
Published
1977-01-01
How to Cite
J. Brouwer. (1977). Depositional environment of the Oligocene Rupel Clay in well Grashoek-l, Peel region, The Netherlands. Netherlands Journal of Geosciences, 25-30. Retrieved from https://njgjournal.nl/index.php/njg/article/view/14287
Issue
Section
Regular paper
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