Knowledge of Nubia/Somalia relative motion since the Early Neogene is of particular importance in the Earth Sciences, because it (i) impacts on inferences on African dynamic topography; and (ii) allows us to link plate kinematics within the Indian realm with those within the Atlantic basin. The contemporary Nubia/Somalia motion is well known from geodetic observations. Precise estimates of the past-3.2-Myr average motion are also available from paleo-magnetic observations. However, little is known of the Nubia/Somalia motion prior to ∼3.2 Ma, chiefly because the Southwest Indian Ridge spread slowly, posing a challenge to precisely identify magnetic lineations. This also makes the few observations available particularly prone to noise. Here ...
The Red Sea and Gulf of Aden represent two young basins that formed between Africa and Arabia since ...
The East African Rift System (EARS) represents a major tectonic feature that splits the African cont...
The Nubia-Somalia boundary is one of the least well defined plate boundaries. The southern extension...
Previous reconstructions for anomaly 5 and older anomalies flanking the Southwest Indian Ridge (SWIR...
Reconstructions of the history of convergence between the Nubia and Eurasia plates constitute an imp...
International audienceSUMMARY We reconstruct the post-52 Ma seafloor spreading history of the Southw...
Present-day continental extension along the East African Rift System (EARS) has often been attribute...
We use geodetic and plate tectonic observations to constrain the tectonic evolution of the Nubia-Ara...
The Red Sea and Gulf of Aden represent two young basins that formed between Africa and Arabia since ...
A refinement and extrapolation of recent motion estimates for the Danakilmicroplate, based on ancien...
The motion of the Somalia plate relative to the Nubia (Africa), Arabia and Antarctica platcs is re-e...
International audienceNew geophysical data collected at the Aden‐Owen‐Carlsberg (AOC) triple junctio...
The Red Sea and Gulf of Aden represent two young basins that formed between Africa and Arabia since ...
The Nubia plate is normally considered to be a rigid plate and as such used in the realization of te...
International audienceWe analyzed 16 years of GPS and 17 years of Doppler orbitography and radioposi...
The Red Sea and Gulf of Aden represent two young basins that formed between Africa and Arabia since ...
The East African Rift System (EARS) represents a major tectonic feature that splits the African cont...
The Nubia-Somalia boundary is one of the least well defined plate boundaries. The southern extension...
Previous reconstructions for anomaly 5 and older anomalies flanking the Southwest Indian Ridge (SWIR...
Reconstructions of the history of convergence between the Nubia and Eurasia plates constitute an imp...
International audienceSUMMARY We reconstruct the post-52 Ma seafloor spreading history of the Southw...
Present-day continental extension along the East African Rift System (EARS) has often been attribute...
We use geodetic and plate tectonic observations to constrain the tectonic evolution of the Nubia-Ara...
The Red Sea and Gulf of Aden represent two young basins that formed between Africa and Arabia since ...
A refinement and extrapolation of recent motion estimates for the Danakilmicroplate, based on ancien...
The motion of the Somalia plate relative to the Nubia (Africa), Arabia and Antarctica platcs is re-e...
International audienceNew geophysical data collected at the Aden‐Owen‐Carlsberg (AOC) triple junctio...
The Red Sea and Gulf of Aden represent two young basins that formed between Africa and Arabia since ...
The Nubia plate is normally considered to be a rigid plate and as such used in the realization of te...
International audienceWe analyzed 16 years of GPS and 17 years of Doppler orbitography and radioposi...
The Red Sea and Gulf of Aden represent two young basins that formed between Africa and Arabia since ...
The East African Rift System (EARS) represents a major tectonic feature that splits the African cont...
The Nubia-Somalia boundary is one of the least well defined plate boundaries. The southern extension...