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

Agor Fm


Period: 
Quaternary

Age Interval: 
Pleistocene - Holocene


Province: 
SouthSudan, Sudan S

Type Locality and Naming

Melut Basin (NE South Sudan - W Ethiopia), and the Rawat Basin (SE Sudan), which are the southeastern and the northwestern basins of the greater White Nile rift basin.

Reference: Dou et al., 2007; Dou et al., 2023 (Melut Basin); Mohammed et al, 2017 (Rawat Basin)

[Fig. 1: Simplified map of the West and Central African Rift System (WCARS) showing the major features discussed in the text and the location of the Melut Basin in South Sudan (modified from Genik, 1993)]

[Fig. 2: Comprehensive stratigraphic columns in the Melut Basin (from Dou et al., 2023)]

[Fig. 3: Rawat Basin- Block 25 in southern Sudan (after Ministry of Petroleum & Gas-OEPA, 2015, Extracted from Mohammed et al., 2017).]

[Fig. 4: Summary of Tectono-stratigraphy of the Rawat Basin (from Mohammed, 2016).]


Lithology and Thickness

In Melut Basin, it is mainly composed of loose sands and clay (Dou et al., 2007).

In Rawat Basin (Mohammed et al, 2017), the Agor Fm is the youngest monotonous sand sequences commonly identified on the tops of all wells in the Rawat Basin. It consists of clay/claystone interbedded with thin layer of sand. The sand is medium to coarse grained, subrounded, subangular, and moderately sorted, occasional pebble sized grains. The clay is dusk yellow, yellowish grey, to pale olive, soft, sticky, amorphous, and slightly calcareous (Hassan, 2016).


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

Agor Fm unconformably overlies the Daga Fm

Upper contact

Present surface

Regional extent

Melut Basin (NE South Sudan - W Ethiopia), and the Rawat Basin (SE Sudan), which are the southeastern and the northwestern basins of the greater White Nile rift basin.


GeoJSON

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Fossils

In Rawat Basin (Mohammet et al, 2017): Spores-Pollen (Concavissimisporites punctatus, Cythiditess australis, Verrucatosporites usmensis, Tricolpites sp., Laevigatosporites haardti)


Age 

Quaternary

Age Span: 

    Beginning stage: 
Gelasian

    Fraction up in beginning stage: 
0.00

    Beginning date (Ma): 
2.58

    Ending stage: 
Holocene

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
0.00

Depositional setting

Progradational period of lacustrine environment (Hassan, 2016).


Depositional pattern:  


Additional Information


Compiler:  

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

Dou L., Xiao K., Cheng D., Shi B., Li Z. (2007): Petroleum Geology of the Melut Basin and the Great Palogue Field, Sudan. Marine and Petroleum Geology, 24, pp.129-144

Dou L., Xiao K., Wang J. (2023): Petroleum Geology and Exploration of the Bongor Basin. Petroleum Industry Press.

Mohammed H. Z. A., Awad M. Z., Eisawi (2017): Upper Cretaceous to Neogene Palynology of the Rawat Basin, White Nile State, Sudan. Journal of Earth Science & Climatic Change. 08 (04)

Robertson Research International “RRI”, Geological Research Authority of Sudan “GRAS” (2016): The Geology and Petroleum Potential of Southern, Central, and Eastern Sudan. Unpublished Report. Vol. 1-4