The Role of Pre-Existing Precambrian Structures in Rift Evolution: The Albertine and Rhino Grabens, Uganda
We integrated Shuttle Radar Topography Mission (SRTM) Digital Elevation Models (DEM), airborne magnetic, radiometric and three-dimensional Full Tensor Gravity Gradiometry (3D-FTG) data to investigate the role of Precambrian structures in the evolution of the largely amagmatic Miocene-Recent aged Albertine and Rhino grabens in Uganda. These grabens represent the northern segment of the Western Branch of the East African Rift System (EARS). The two NE-trending grabens are connected by a right-stepping transfer zone and they extend within the Archean-Paleoproterozoic Northeast Congo block which represents the northeastern extension of the Congo craton. Our results show the following and highlight the importance of pre-existing structures in the evolution of continental rift systems: (1) The NE-extent of the Albertine full-graben is controlled by NE-trending Precambrian fabric and the graben terminates at its northeastern end when it encounters a multiply folded Precambrian basement terrain with poorly-developed NW-trending structural grain. Additionally, the northeastern termination of the Albertine graben coincides with the presence of NW-trending right-stepping high-density bodies within the Precambrian terrain. (2) The transfer zone between the Albertine and Rhino grabens is controlled by NE-trending Precambrian structures which might have facilitated the development of relay ramp faults. (3) Strain localization within the better-developed southeastern border fault of the Rhino half-graben is facilitated by the presence of Precambrian structures better aligned in a NE-direction in the southeastern part of the basin compared to its northwestern part. (4) Further to the northeast, the Rhino graben is segmented and transitions into a narrower ENE-trending half-graben with a better-developed border fault on its northwestern side. This segmentation coincides with the presence of N-trending Precambrian structures. (5) The Rhino graben terminates farther northeast against the NW-trending Precambrian Aswa shear zone; a prominent structure with complex, but generally NW-trending fabric.
A. B. Katumwehe et al., "The Role of Pre-Existing Precambrian Structures in Rift Evolution: The Albertine and Rhino Grabens, Uganda," Tectonophysics, vol. 646, pp. 117-129, Elsevier, Apr 2015.
The definitive version is available at https://doi.org/10.1016/j.tecto.2015.01.022
Geosciences and Geological and Petroleum Engineering
National Science Foundation (U.S.)
Keywords and Phrases
Geologic Models; Tracking Radar; Amagmatic Rifts; Digital Elevation Model; East African Rift; Existing Structure; Prominent Structures; Rhino And Albertine Grabens; Shuttle Radar Topography Mission; Strain Localizations; Surveying; Craton; Graben; Precambrian; Rift Zone; Shear Zone; Tectonic Evolution; Tectonic Structure; Uganda; East African Rift System; Pre-existing Structures
International Standard Serial Number (ISSN)
Article - Journal
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