Home Multi-Country Search About Admin Login
Cenozoic
Mesozoic
Paleozoic
Neoproterozoic
Paleoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Galamboge Formation
Click to display on map of the Ancient World at:
Galamboge Fm base reconstruction

Galamboge Fm


Period: 
Ediacaran

Age Interval: 
Latest Ediacaran


Province: 
Northern Congo Margin

Type Locality and Naming

Lower unit of the Aruwima Gr. Exposed along the Aruwimi River near Yambuya.

Synonym: Galamboge Quartzites, Galamboge Subgroup

Reference: De Wit et al., 2015;Kadima et al., 2011; Trompette,1994;Sechse et al., 2011

[Fig 1. Simplified geological map of the Congo Basin, compiled from various published map. The stratigraphic units have been assembled into major sequences (Late Neoproterozoic, Paleozoic and Cenozoic)]

[Fig 2. Tectonic setting of the Neoproterozoic basins of present-day Central Africa, compiled from the 1: 2M geological map of the Zaire (Lepersonne, 1974) and the 1: 4M map Geology and Major Ore Deposits of Africa (Milesi et al., 2006)]

[Fig 3. Lithostratigraphic synthesis for the Neoproterozoic to Early Paleozoic period. Compiled after various authors. Dotted lines between Banalia, Alolo and Galamboge formations: stratigraphic transition by recurrences]

[Fig 4. Lithostratigraphic columns for the Congo Basin established using data from the 4 wells in the central part of the basin and outcrops on its NE margin (Lindi-Ubangi and Kisangani-Kindu region), compared with the West-Congo and Katanga stratigraphy]

[Fig 5.Simplified geological map of Sub-Saharan Africa showing the Neoproterozoic basins on and around the Congo Shield (modified after De Waele et al. 2008). (LC) Lower Congo Basin, (Co) Comba Basin, (Sa) Sangha Basin, (Ny) Nyanga-Niari Basin, (An) Angola Basin, (SO) Semb-Ouesso Basin, (Ba) Ubangui Basin, (LiB) Likki-Bembe´ Basin, (Bk) Bakouma Basin, (Fou) Fouroumbala Basin, (Li) Lindi Basin, It Itombwe Basin, (Ma)Malagarazi-Bukoban Basin, (Mb) Sankuru-Mbuji-Mayi-Lomami-Lovoy Basin, (Lu) Luamba Group, (Kat) Katanga Basin, (RB) Ruwenzorian Belt, KaB) Karagwe-Ankole Belt, (RuB) Ruzisian Belt, (KiB) Kibaran Belt,(UB) Ubendian Belt, IB Irumide Belt]

[Fig 6.Northern margin of the Congo Shield. (A) Geological sketch map of the Lindi Basin (modified after Verbeek 1970; Poidevin 1985)]

[Fig 7. Stratigraphic logs of the Lindi Supergoup in the DRC (modified after Verbeek 1970). (C and D) Stratigraphic logs of the Lindi Supergoup in CAR (modified after Poidevin 1985). cc cap carbonates, SG Sturtian Glaciation, MG Marinoan Glaciation]

[Fig 8. Stratigraphic correlation between the Neoproterozoic sedimentary basins in Central Africa. Correlations based on Sr isotopic data, radiometric age constraints and revised lithological relationships]


Lithology and Thickness

The Galamboge Quartzites consists of 100-150m of reddish brown to whitish, massive, medium-grained quartzites and quartzitic sandstones, generally displaying cross-bedding. At the bottom, some conglomeratic layers are observed. Interbedded micaceous reddish brown argillaceous shales occur both in the upper and lower parts of the unit. The Galamboge Quartzites contain variable amount of feldspar and clasts of rocks.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Lies unconformably on the Lokoma Gr

Upper contact

Overlain by the Alolo Fm (upper unit of the Aruwimi Gr)

Regional extent

Extends to the Lindi Basin of the northeastern DRC. Trompette (1994) considered this basin and Fouroumbala-Bakouma basins of the south-western CAR, and to be part of the Lindi Basin.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[21.89,3.94],[23.36,3.92],[26.92,2.7],[26.79,3.14],[27.5,2.84],[29.65,3.19],[29.99,2.33],[28.36,0.65],[27.4,0.7],[26.18,0.99],[25.01,1.58],[23.45,2.72],[21.87,3.41],[21.11,3.97],[21.89,3.94]]]]}}

Fossils


Age 

arbitrarily put as the latest Ediacaran portion of the Aruwima Gr for graphic purposes

Age Span: 

    Beginning stage: 
Ediacaran

    Fraction up in beginning stage: 
0.85

    Beginning date (Ma): 
553.23

    Ending stage: 
Ediacaran

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
538.80

Depositional setting

Continental, fluviatile, Aeolian environment (Kadima et al., 2011)


Depositional pattern:  


Additional Information


Compiler:  

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

Geology and Resource Potential of the Congo Basin by Maarten J. de Wit, François Guillocheau and Michiel C.J. de Wit, Published Springer-Verlag Berlin Heidelberg 2015; DOI 10.1007/978-3-642-29482-2

Kadima, E., Delvaux, D., Sebagenzi, S.N., Tack, L., Kabeyaz (2011). Structure and geological history of the Congo Basin: an integrated interpretation of gravity, magnetic and reflection seismic data Basin Research (2011) 23, 499–527, doi: 10.1111/j.1365-2117.2011.00500.x