Home Multi-Country Search About Admin Login

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Mikambeni Formation

Mikambeni Fm


Period: 
Permian

Age Interval: 
Middle-Late Permian (Roadian-Changhsingian)


Province: 
SouthAfrica-Namibia-Botswana

Type Locality and Naming

Soutpansberg, Tshipise, Pafuri, and Tuli Basins (Limpopo Province, South Africa). Named after the Mikambeni feature in the northern Limpopo Province of South Africa. Upper formation in Ecca Gr in Tshipise Basin

Synonym:


Lithology and Thickness

A predominantly fine-grained, argillaceous succession reaching thicknesses of approximately 20 to 140 meters. It consists almost entirely of dark grey to black, highly carbonaceous shales, massive mudstones, and finely laminated micaceous siltstones. It also contains minor, very thin (and generally uneconomic) coal stringers and occasional lenticular, fine-grained sandstone beds.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

Conformably and transitionally overlies the heavily alternating sandstones, shales, and thick economic coal seams of the Madzaringwe Fm (the basal Ecca Gr equivalent in the region).

Upper contact

Conformably, but frequently sharply, overlain by the prominent, coarse-grained, white arkosic sandstones of the Fripp Fm

Regional extent

Restricted geographically to the ENE-WSW trending, fault-bounded Karoo rift basins of northern South Africa (the Soutpansberg, Tshipise, Pafuri, and Tuli basins), stretching eastward into the northern Kruger National Park. Middle to Upper Ecca Gr equivalent in the northern rift basins. It is the regional chronostratigraphic equivalent of the upper Vryheid Fm and lower Volksrust Fm in the Main Karoo Basin, and broadly correlates with parts of the Grootegeluk Fm in the Ellisras Basin.


GeoJSON

null

Fossils


Age 

Middle-Late Permian (Roadian-Changhsingian)

Age Span: 

    Beginning stage: 
Roadian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
274.37

    Ending stage: 
Changhsingian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
251.90

Depositional setting

Shallow lacustrine (lake) and extensive paludal (swamp) to floodplain environments.


Depositional pattern:  


Additional Information


Compiler:  

From the O. Catuneanu et al. / Journal of African Earth Sciences 43 (2005) 211–253; Brandl, G. (1981): The geology of the Messina area. Explanation of Sheet 2230, Geological Survey of South Africa; Johnson, M.R., et al. (2006): Sedimentary rocks of the Karoo Supergroup. In: The Geology of South Africa; Malaza, N., et al. (2013): Organic petrology and geochemistry of the coal-bearing Madzaringwe and Mikambeni Formations...