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Information provided by geoscience team at Ahmadu Bello University, Zaria, Nigeria --see About

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Tendi Formation
Click to display on map of the Ancient World at:
Tendi Fm base reconstruction

Tendi Fm


Period: 
Neogene

Age Interval: 
Early and Middle Miocene


Province: 
Sudan S

Type Locality and Naming

Muglad Basin -- SW Sudan and the northwestern part of South Sudan. Lower-middle formation of the Kordofan Gr.

Reference: Babikir, 1997; Makeen et al., 2013; Jingyao, 2015; Ahmed and Ozumba, 2017

[Fig. 1: Western and Central African rift system. West African rift subsystem and Central African]

[Fig. 2: General stratigraphic column - Muglad Basin, Sudan, showing three geological cycles – Neocomian to Barremian, Aptian to Maastrichtian, and Paleocene to Pliocene - Miocene, or Quaternary and Petroleum Systems (from Ahmed and Ozumba, 2017)]

[Fig. 3: Comprehensive stratigraphic columns in the Muglad Basin (from Dou et al., 2023)]

[Fig. 4: Regional stratigraphy of the Muglad basin, SW Sudan (after Schull 1988; Dou Lirong et al. 2013 – extracted from Makeen et al., 2013)]

[Fig. 5: Location map of the Fula sub-basin in the Muglad basin including oilfields (study area) (after Dou Lirong et al. 2013 – extracted from Makeen et al., 2013)]


Lithology and Thickness

The Tendi Formation is predominantly made up of shales and has an estimated thickness of 1950m (Makeen et al., 2013; Jingyao, 2015)


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

conformably rests on the Nayil Fm

Upper contact

Adok Fm conformably rests on the Tendi Fm

Regional extent

Muglad Basin -- SW Sudan and the northwestern part of South Sudan


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[24.03,11.51],[28.25,12.97],[28.62,12.44],[28.81,11.05],[29.84,10.63],[30.84,8.68],[32.79,5.97],[33.11,5.02],[32.01,4.83],[30.98,6.02],[28.91,7.46],[26.91,9.09],[23.42,10.39],[23.4,11.09],[24.03,11.51]]]]}}

Fossils

Pollens (Cyathidites minor-Perfotricolpites digitatus)


Age 

Early and Middle Miocene

Age Span: 

    Beginning stage: 
Aquitanian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
23.04

    Ending stage: 
Tortonian

    Fraction up in the ending stage: 
0.0

    Ending date (Ma):  
11.63

Depositional setting

lacustrine as well as fluvial overbank depositional setting (Ahmed and Ozumba, 2017).


Depositional pattern:  


Additional Information


Compiler:  

Enam O. Obiosio, Solomon Joshua Avong and Henry Nasir Suleiman (2024) - Stratigraphic Lexicon compiled from the following books:

Dou D., Dingsheng C., Zhi L., Zhiwei Z., Jingchun W. (2013): Petroleum Geology of the Fula Sub-Basin, Muglad Basin, Sudan. Journal of Petroleum Geology, 36(1): pp.43-60

Jingyao W. (2015): The Study of Sequence Stratigraphy and Sedimentary System in Muglad Basin. IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG), 3(6): pp.37-40

Makeen Y. M., Abdullah W. H., Hakimi M. H. (2013): Biological markers and organic petrology study of organic matter in the Lower Cretaceous Abu Gabra sediments (Muglad Basin, Sudan): origin, type and palaeoenvironmental conditions. Arabian Journal of Geosciences. DOI 10.1007/s12517-013-1203-z

Lenhardt, N., Omietimi, E. J., Edegbai, A. J., Schwark, L., Catuneanu, O., Fairhead, J. D., Gotz, A. E. (2025): Traversing the rift: A review of the evolution of the West and Central African Rift System and its economic potential. Earth-Science Reviews, 261: pp. 1-39