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  • 1
    Publication Date: 2020-06-03
    Description: Continental rift systems form by propagation of isolated rift segments that interact, and eventually evolve into continuous zones of deformation. This process impacts many aspects of rifting including rift morphology at breakup, and eventual ocean-ridge segmentation. Yet, rift segment growth and interaction remain enigmatic. Here we present geological data from the poorly documented Ririba rift (South Ethiopia) that reveals how two major sectors of the East African rift, the Kenyan and Ethiopian rifts, interact. We show that the Ririba rift formed from the southward propagation of the Ethiopian rift during the Pliocene but this propagation was short-lived and aborted close to the Pliocene-Pleistocene boundary. Seismicity data support the abandonment of laterally offset, overlapping tips of the Ethiopian and Kenyan rifts. Integration with new numerical models indicates that rift abandonment resulted from progressive focusing of the tectonic and magmatic activity into an oblique, throughgoing rift zone of near pure extension directly connecting the rift sectors.
    Description: This research was supported by the National Geographic Society (Grant #9976–16, P.I. G. Corti). We thank the DigitalGlobe Foundation for providing the satellite image in Fig. 3. We warmly thank Antonio Zeoli for the processing of the satellite images and Pablo Tierz for valuable discussions. Inversion of fault-slip data and volcanic alignments was obtained using Win-Tensor, a software developed by Dr. Damien Delvaux, Royal Museum for Central Africa, Tervuren, Belgium. D.K. is supported by NERC grant NE/ L013932. F.I.-K. is supported by the ECLIPSE Program funded by the New Zealand Ministry of Business, Innovation and Employment. S.B. and A.G. are supported by the Helmholtz Young Investigators Group CRYSTALS (VH-NG-1132). Numerical models were conducted on HLRN cluster Konrad. The Ar/Ar laboratory at ISTO is supported by LABEX Grant “VOLTAIRE”.
    Description: Published
    Description: id 1309
    Description: 1T. Struttura della Terra
    Description: JCR Journal
    Keywords: Ririba Rift ; South Etiopia
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2021-09-29
    Description: Complex, time‐dependent, and asymmetric rift geometries are observed throughout the East African Rift System (EARS) and are well documented, for instance, in the Kenya Rift. To unravel asymmetric rifting processes in this region, we conduct 2D geodynamic models. We use the finite element software ASPECT employing visco‐plastic rheologies, mesh‐refinement, distributed random noise seeding, and a free surface. In contrast to many previous numerical modeling studies that aimed at understanding final rifted margin symmetry, we explicitly focus on initial rifting stages to assess geodynamic controls on strain localization and fault evolution. We thereby link to geological and geophysical observations from the Southern and Central Kenya Rift. Our models suggest a three‐stage early rift evolution that dynamically bridges previously inferred fault‐configuration phases of the eastern EARS branch: (1) accommodation of initial strain localization by a single border fault and flexure of the hanging‐wall crust, (2) faulting in the hanging‐wall and increasing upper‐crustal faulting in the rift‐basin center, and (3) loss of pronounced early stage asymmetry prior to basinward localization of deformation. This evolution may provide a template for understanding early extensional faulting in other branches of the East African Rift and in asymmetric rifts worldwide. By modifying the initial random noise distribution that approximates small‐scale tectonic inheritance, we show that a spectrum of first‐order fault configurations with variable symmetry can be produced in models with an otherwise identical setup. This approach sheds new light on along‐strike rift variability controls in active asymmetric rifts and proximal rifted margins.
    Description: Key Points: 2D numerical models elucidate evolution of asymmetric Kenya Rift segments. Intrabasinal faulting is caused by bending of the central block and does not reach the brittle‐ductile transition. Small‐scale crustal inheritance can exert decisive control on first‐order rift architecture.
    Description: Helmholtz Young Ivestigators Group
    Description: National Science Foundation
    Keywords: 551.8 ; 556 ; asymmetric rifting ; rift variability ; numerical model ; structural inheritance ; Kenya Rift
    Type: map
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