Tevrede Fm
Type Locality and Naming
Waterberg-Erongo area, central Namibia. It was formally identified and described from borehole cores by Gunthorpe (1987). Included in Ecca Gr in Waterberg Basin.
Synonym:
Lithology and Thickness
Approximately 40 meters thick. The succession comprises glauconite-bearing mudstones, sandstones, and coal seams.
Relationships and Distribution
Lower contact
Unconformably overlies the Neoproterozoic Damara basement rocks, though it may speculatively rest on thin, highly localized glaciogenic Dwyka equivalents in the deepest parts of the basin.
Upper contact
Unconformably overlain by the Early Triassic fluvial red beds of the Lower Omingonde Fm. This contact is a major disconformity (marked by a pedogenically modified paleosol surface at the top of the Tevrede) representing a massive depositional hiatus of up to 40 million years.
Regional extent
Regional equivalent of the Lower Permian Ecca Gr (and potentially uppermost Dwyka Gr) within the fault-bounded Waterberg Basin. Restricted to the subsurface of the Waterberg-Erongo Basin in central Namibia. Due to its stratigraphic position and the overlying unconformity, it rarely outcrops and is known almost exclusively from drill cores.
GeoJSON
Fossils
Age
Depositional setting
Additional Information