A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a 10-day period, c. 2.5 km3 of magma were intruded into the upper crust along a 60 km-long dyke separating the Arabian and Nubian plates. There was an intense seismic swarm and a small rhyolitic eruption; extension of up to 10 m occurred across the rift segment. Over the next five years, a further 13 dyke intrusions caused continued extension, eruptions and seismicity. The activity in Afar led to a renewed international focus on the role of magmatism in rifting, with major collaborative projects involving researchers from Ethiopia, the UK, the USA, France, Italy and New Zealand working in Afar and Ethiopia to study the ongoing activity and to place...
[ 1] The volcanically active Main Ethiopian rift ( MER) marks the transition from continental riftin...
Magma along divergent plate boundaries is erupted from fissures or vents from central volcanoes, wit...
International audience[1] We seek to characterize how magmatic and tectonic activities combine and i...
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a 10-d...
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a ten-...
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a 10-d...
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a 10-d...
Rift zones are the most common magmatic environment on Earth. However opportunities to observe activ...
Rift zones are the most common magmatic environment on Earth. However opportunities to observe activ...
Rift zones are the most common magmatic environment on Earth. However opportunities to observe activ...
Riftzones are the most common magmatic environment on Earth. However opportunities to observe active...
Although fault and magmatic processes have achieved plate spreading at mid-ocean ridges throughout E...
Continental rupture models emphasize the role of faults in extensional strain accommodation; extensi...
Continental rupture models emphasize the role of faults in extensional strain accommodation; extensi...
The Dabbahu-Manda Hararo rift segment is a ~25 x 60 km rift zone in Afar, Ethiopia, where a series o...
[ 1] The volcanically active Main Ethiopian rift ( MER) marks the transition from continental riftin...
Magma along divergent plate boundaries is erupted from fissures or vents from central volcanoes, wit...
International audience[1] We seek to characterize how magmatic and tectonic activities combine and i...
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a 10-d...
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a ten-...
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a 10-d...
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a 10-d...
Rift zones are the most common magmatic environment on Earth. However opportunities to observe activ...
Rift zones are the most common magmatic environment on Earth. However opportunities to observe activ...
Rift zones are the most common magmatic environment on Earth. However opportunities to observe activ...
Riftzones are the most common magmatic environment on Earth. However opportunities to observe active...
Although fault and magmatic processes have achieved plate spreading at mid-ocean ridges throughout E...
Continental rupture models emphasize the role of faults in extensional strain accommodation; extensi...
Continental rupture models emphasize the role of faults in extensional strain accommodation; extensi...
The Dabbahu-Manda Hararo rift segment is a ~25 x 60 km rift zone in Afar, Ethiopia, where a series o...
[ 1] The volcanically active Main Ethiopian rift ( MER) marks the transition from continental riftin...
Magma along divergent plate boundaries is erupted from fissures or vents from central volcanoes, wit...
International audience[1] We seek to characterize how magmatic and tectonic activities combine and i...