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Shendi Formation
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Shendi Fm base reconstruction

Shendi Fm


Period: 
Cretaceous

Age Interval: 
midCampanian - Maastrichtian


Province: 
Sudan E

Type Locality and Naming

Atbara Basin, east of Blue Nile Basin, East Sudan

Kheiralla (1966) introduced the name Quartoze Sandstone to describe the siliciclastic rocks cropping out in Shendi area (Abujaball et al., 2021). A formal lithostratigraphic nomenclature of the units was given by Whiteman (1971) who proposed the name Shendi formation whose type locality is represented by outcrops north east of kabushiya village, River Nile state (Abujaball et al., 2021).

References:

[Fig. 1: Tectonic model of the West and Central African Rift System (WCARS) and the Central African Shear Zone (CASZ). The red arrow and rectangle represent the Shendi-Atbara Basin and study area (Modified after Fairhead, 1988b).]

[Fig. 2: Stratigraphy of the CARS (modified from Schull, 1988; McHargue et al., 1992; Guiraud and Bosworth, 1997; Gani et al., 2009; Wolela, 2009; Dou et al., 2013, 2018, 2023a; Liu and Chen, 2014; Eisawi et al., 2015; Mohammed et al., 2016; Bussert et al., 2018; Yassin et al., 2017; Mohammed Yasin et al., 2019; Gao et al., 2023)]

[Fig. 3. Stratigraphic chart of Shendi-Atbara Basin showing the rock units succession and the basin evolution (from Babkir et al., 2023).]

[Fig. 4. Map showing the location of WCARS basins in between major cratonic areas in Africa, including the subdivision into a Western, Arabian-Nubia, and Southern Austral block (modified from Genik, 1993; Meert and Lieberman, 2008).]


Lithology and Thickness

The formation is dominated by sandstones with a few shale beds (Fig. 9 of Lenhardt et al., 2025). Kheiralla (1966) described the Shendi Formation as being composed of pebble conglomerates, intraformational conglomerates, sandstones, and mudstones. The sandstones were described as well-bedded, non-pebbly, clean, and very well-sorted, consisting mainly of quartz grains cemented with iron oxides (Kheiralla, 1966). The Shendi Formation has been formally subdivided into two member: the umm Ali member and the Kabushiya member (Abujaball et al., 2021).


Lithology Pattern: 
Aus conglomerate


Relationships and Distribution

Lower contact

Mahmiya Fm, conformably

Upper contact

Wadi Awatib – Hudi Chert Fm, unconformably (Paleocene is absent)

Regional extent

Atbara Basin, Sudan


GeoJSON

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Fossils

Pollen (Abujaball et al., 2021)


Age 

lower-middle Campanian through Maastrichtian (strat column of Lenhardt et al., 2025)

Age Span: 

    Beginning stage: 
Campanian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
79.06

    Ending stage: 
Maastrichtian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
66.04

Depositional setting

Fluvial setting (Babkir et al., 2023). Lacustrine to fluvial-lacustrine condition (Abujaball et al., 2021). Bussert (1998) reported that the Shendi Formation was deposited in a fluviatile system, mainly of braided and meandering nature. It is believed that such fluviatile systems changed gradually, with time, from braided into meandering river systems by the Late Cretaceous (Bussert, 1998). Moreover, lacustrine sedimentation as a result of post-rift activities was also reported in some parts of the basin (Klitzsch and Squyres, 1990; Oshi, 2004).


Depositional pattern:  


Additional Information


Compiler:  

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

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

Babkir, M.D.B.H., Nton, M.E., Eisawi, A.A.M. (2023): Depositional environment and hydrocarbon exploration potential based on sedimentary facies and architectural analysis of the Upper Cretaceous Shendi Formation in Musawwarat-Naga area, Shendi-Atbara Basin, Sudan. Earth Sci. Research Jour., 27(2): 109-128