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This research includes the use of seismic data, well logs and dinocyst palynology. Results reveal a migration of the depocentre towards the north-west in the late Miocene. The Diessen Formation can be subdivided into four units that can be regionally correlated. The mid-Miocene unconformity has caused large incisions in the structural highs. No hiatus associated with the mid-Miocene unconformity is present in the central Roer Valley Graben.
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