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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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40Ar/39Ar thermochronology of the Ethiopian and Yemeni basements: reheating related to the Afar plume?

TL;DR: In this paper, a 40 Ar/39 Ar thermochronological study has been carried out on the Panafrican basement in Ethiopia and Yemen using the furnace step heating procedure.
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The making of an underplate: Pyroxenites from the Ethiopian lithosphere

TL;DR: In this article, a petrographic and geochemical study of pyroxenite xenoliths erupted on the western Ethiopian plateau from along the Yerer Tullul Wellel Volcano-Tectonic lineament (YTVL).
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Fluidal pyroclasts reveal the intensity of peralkaline rhyolite pumice cone eruptions.

TL;DR: It is shown that peralkaline rhyolite pumice cones are the product of moderate to intense eruptions, meaning that such eruptions can generate extensive tephra-fall and pyroclastic density currents.
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Stability of rift axis magma reservoirs: Spatial and temporal evolution of magma supply in the Dabbahu rift segment (Afar, Ethiopia) over the past 30 kyr

TL;DR: In this paper, a combination of cosmogenic (36Cl and 3He) surface exposure dating of basaltic lava-flows, field observations, geological mapping and geochemistry was used to uncover the volcanic history of the Dabbahu/Manda Hararo rift segment in the Afar depression (Ethiopia).
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Constraining timescales of focused magmatic accretion and extension in the Afar crust using lava geochronology

TL;DR: It is shown that lavas, which erupted since ~200 ka along part of the on-land Red Sea rift system in Afar, Ethiopia, have a consistent age-progression from the rift axis outwards, indicating that axial dyke intrusion has been the primary mechanism of segment growth and that focused magmatic accretion and extension in the crust have remained stable here over this period.