GPS observations along three profiles across the Ethiopian Rift and Afar triple junction record differences in the length scale over which extension is accommodated. In the Afar region, where the mantle lithosphere is nearly or entirely absent, measurable extension occurs over ∼175 km; in the northern Ethiopian Rift, where the mantle lithosphere is anomalously thin and hot, extensional strain occurs over ∼85 km, extending beyond the structural rift valley; in the southern Ethiopian Rift, where the mantle lithosphere approaches standard continental thickness, extensional strain occurs over <10 km. This trend of increasingly distributed deformation contrasts with the standard model where continental rifts become mid-ocean spreading centers th...
Strain and seismicity show us the mode by which deformation is accommodated in rifting continents. H...
International audienceThe extension of continental lithosphere is usually classified into three mode...
The transition from continental rifting to seafloor spreading is a key, yet enigmatic, stage of the ...
As rifting progresses to seafloor spreading, extension within the continental crust commonly is acco...
International audienceImaging the lithosphere is key to understand mechanisms of extension as riftin...
Rifting of the continents leading to plate rupture occurs by a combination of mechanical deformation...
Imaging the lithosphere is key to understand mechanisms of extension as rifting progresses. Continen...
Continental extension is caused by a combination of mechanisms such as mechanical stretching, thinni...
The kinematics of rift segment linkage in magmatic rifts remain debated. Strain patterns from Afar p...
We present the kinematics of the Ethiopian Rift, in the northern part of East African Rift System, d...
In this study we image crustal structure beneath a magmatic continental rift to understand the inter...
Lithospheric strength and strain localization in continental extension from observations of th
Imaging the lithosphere is key to understand mechanisms of extension as rifting progresses. Continen...
In this study we image crustal structure beneath a magmatic continental rift to understand the inter...
International audienceKinematics of divergent boundaries and Rift-Rift-Rift junctions are classicall...
Strain and seismicity show us the mode by which deformation is accommodated in rifting continents. H...
International audienceThe extension of continental lithosphere is usually classified into three mode...
The transition from continental rifting to seafloor spreading is a key, yet enigmatic, stage of the ...
As rifting progresses to seafloor spreading, extension within the continental crust commonly is acco...
International audienceImaging the lithosphere is key to understand mechanisms of extension as riftin...
Rifting of the continents leading to plate rupture occurs by a combination of mechanical deformation...
Imaging the lithosphere is key to understand mechanisms of extension as rifting progresses. Continen...
Continental extension is caused by a combination of mechanisms such as mechanical stretching, thinni...
The kinematics of rift segment linkage in magmatic rifts remain debated. Strain patterns from Afar p...
We present the kinematics of the Ethiopian Rift, in the northern part of East African Rift System, d...
In this study we image crustal structure beneath a magmatic continental rift to understand the inter...
Lithospheric strength and strain localization in continental extension from observations of th
Imaging the lithosphere is key to understand mechanisms of extension as rifting progresses. Continen...
In this study we image crustal structure beneath a magmatic continental rift to understand the inter...
International audienceKinematics of divergent boundaries and Rift-Rift-Rift junctions are classicall...
Strain and seismicity show us the mode by which deformation is accommodated in rifting continents. H...
International audienceThe extension of continental lithosphere is usually classified into three mode...
The transition from continental rifting to seafloor spreading is a key, yet enigmatic, stage of the ...