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Gezahegn Yirgu

Researcher at Addis Ababa University

Publications -  84
Citations -  6221

Gezahegn Yirgu is an academic researcher from Addis Ababa University. The author has contributed to research in topics: Rift & Volcano. The author has an hindex of 35, co-authored 75 publications receiving 5428 citations.

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Isotopic and trace element signatures of Ethiopian flood basalts: evidence for plume–lithosphere interactions

TL;DR: In this article, trace element and radiogenic isotope data have been measured on Oligocene flood basalts from the northwestern Ethiopian plateau to investigate and identify the nature of mantle and crustal sources involved in the genesis of this huge volume of prerift basalts to constrain the interaction between the Afar mantle plume and the lithosphere at the onset of continental break-up.
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Evolution of a volcanic rifted margin: Southern Red Sea, Ethiopia

TL;DR: In this paper, a structural and stratigraphic framework for the southernmost Red Sea passive margin using new and existing 40 Ar/39 Ar age data along 6 transects is presented.
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The northwestern Ethiopian Plateau flood basalts: Classification and spatial distribution of magma types

TL;DR: In this paper, the authors used trace element data to identify distinct geochemical groups and evaluate the role of differentiation processes in the discovery of low-Ti basalts in the Afro-Arabian CFB province.
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Length and Timescales of Rift Faulting and Magma Intrusion: The Afar Rifting Cycle from 2005 to Present

TL;DR: In this paper, the authors synthesize ongoing seismic, structural, space-based geodetic, and petrologic studies from the subaerial Red Sea rift in Ethiopia where a major rifting episode commenced in September 2005.
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Source, genesis and timing of giant ignimbrite deposits associated with Ethiopian continental flood basalts

TL;DR: The Ethiopian continental flood basalt (CFB) province as discussed by the authors was formed as the result of the impingement of the Afar mantle plume beneath the Ethiopian lithosphere, which includes major sequences of rhyolitic ignimbrites.