The Jurassic Stanleyville formation in the eastern margin of the Congo basin: an example of a shallow balanced-fill lake basin
| dc.contributor.author | Caillaud, A. | |
| dc.contributor.author | Blanpied, C. | |
| dc.contributor.author | Guillocheau, F. | |
| dc.contributor.author | Delvaux, D. | |
| dc.coverage.spatial | Africa - Central | |
| dc.coverage.spatial | Congo, The Democratic Republic of the | |
| dc.coverage.temporal | Jurassic | |
| dc.date | 2017 | |
| dc.date.accessioned | 2024-03-14T13:14:45Z | |
| dc.date.available | 2024-03-14T13:14:45Z | |
| dc.identifier.uri | https://orfeo.belnet.be/handle/internal/11934 | |
| dc.description | The intracratonic Congo Basin, located in the Democratic Republic of Congo (DRC), is the largest sedimentary basin of Africa. The Jurassic strata outcrop along its eastern margin, south of Kisangani (formerly Stanleyville). In the last century, the Upper Jurassic Stanleyville Group was described as a lacustrine series containing a thin basal marine limestone designed as the Lime Fine beds. Since the proposal of this early model, the depositional environment of the Stanleyville Group, and especially the possible marine incursion, has been debated, but without re-examining the existing cores, outcrop samples and historical fossils from the type location near Kisangani that are available at the Royal Museum for Central Africa (MRAC/KMMA, Tervuren, Belgium). In order to refine the former sedimentology, a series of nine exploration cores drilled in the Kisangani sub-basin have been described. This study aims at integrating sedimentary facies in existing sedimentary models and to discuss the hypothesis of the presence of Kimmeridgian marine deposits along the Congo River near Kisangani, a region which lies in the middle of the African continent. Eight facies have been identified, which permit a reinterpretation of the depositional environment and paleogeography of the Stanleyville Group. The base of the Stanleyville Group is interpreted to represent a conglomeratic fluvial succession, which filled an inherited Triassic paleotopography. Above these conglomerates, a transition to a typically lacustrine system is interpreted, which includes: (1) a basal profundal, sublittoral (brown to dark fine-grained siltstones with microbial carbonates, i.e., the Lime Fine beds) and littoral lacustrine series; covered by (2) a sublittoral to profundal interval (brown to dark organic-rich, fine-grained siltstones), which corresponds to the maximum extent of the paleo-lake; and, finally (3) a shallow lacustrine series (greenish calcareous siltstones and sandstones with red siltstones). Unlike what has been proposed, the Lime Fine beds are interpreted herein to be of lacustrine origin, rather than representing a Kimmeridgian marine transgression. We conclude that a Jurassic marine transgression did not, in fact, occur in the eastern region of the Congo Basin. | |
| dc.language | eng | |
| dc.publisher | Elsevier | |
| dc.title | The Jurassic Stanleyville formation in the eastern margin of the Congo basin: an example of a shallow balanced-fill lake basin | |
| dc.type | Article | |
| dc.subject.frascati | Earth and related Environmental sciences | |
| dc.audience | Scientific | |
| dc.subject.free | Geodynamics and mineral resources | |
| dc.source.title | Journal of African Earth Sciences | |
| dc.source.volume | 132 | |
| dc.source.page | 80-98 | |
| Orfeo.peerreviewed | Yes | |
| dc.identifier.doi | 10.1016/j.jafrearsci.2017.05.002 | |
| dc.identifier.url | http://www.sciencedirect.com/science/article/pii/S1464343X17301838 | |
| dc.identifier.rmca | 4993 |