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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
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  • 2
    Publication Date: 2023-11-16
    Description: The relationships between volcanic activity and tectonics at the southernmost termination of the Main Ethiopian Rift (MER), East Africa, still represent a debated problem in the MER evolution. New constraints on the timing, evolution and characteristics of the poorly documented volcanic activity of the Dilo and Mega volcanic fields (VF), near the Kenya-Ethiopia border are here presented and discussed. The new data delineate the occurrence of two distinct groups of volcanic rocks: 1) Pliocene subalkaline basalts, observed only in the Dilo VF, forming a lava basement faulted during a significant rifting phase; 2)Quaternary alkaline basalts, occurring in the twovolcanic fields as pyroclastic products and lava flows issued frommonogenetic edifices and covering the rift-related faults. 40Ar/39Ar dating constrains the emplacement time of the large basal lava plateau to ~3.7 Ma, whereas the youngest volcanic activity characterising the twoareas dates back to 134 ka (Dilo VF) to as recent as the Holocene (Mega VF). Volcanic activity developed along tectonic lineaments independent from those of the rift. No direct relations are observed between the Pliocene, roughly N-S-trending major boundary faults of the Ririba rift and the NE-SW-oriented structural trend characteristic of the Quaternary volcanic activity. We speculate that this change in structural trend may be the expression of (1) inherited crustal structures affecting the distribution of the recent volcanic vents, and (2) a local stress field controlled by differences in crustal thickness, following a major episode of reorganization of extensional structures in the region due to rift propagation and abandonment
    Description: Published
    Description: 106989
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Keywords: Volcano-tectonic activity ; Continental rifting ; Rift evolution ; Inherited fabrics ; 40Ar/39Ar dating ; South Ethiopia ; evolution of rifting in South Ethiopia
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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