International audienceTransform continental margins play a major role in plate tectonics. In the last 10 years' petroleum exploration has moved to the hunt of stratigraphic traps in the passive margin sequence of continent-ocean transforms. The result has been a drastic increase in modern deep seismic data and more well calibrations. Considered as one of the longest continental transform plate boundaries, the Davie transform system (East of Africa) is one of the best places to investigate the evolution of a major transform linking two oceanic basins. Based on a new basement and structural maps and schematic cross-sections, our findings show that the Davie Fracture Zone (DFZ) is made of several transform segments with two main trending direc...
Giant shear processes shaped Africa's southern margin during the break-up of the supercontinent Gond...
Accurate mapping of first-order tectonic features such as oceanic fracture zones and continental mar...
The Gondwana breakup along the Mozambique continental margin caused the formation of extensional and...
Transform continental margins play a major role in plate tectonics. In the last 10 years' petroleum ...
The Davie Ridge is the central morphological element of the Mozambique Channel between East Africa a...
International audienceGondwana splitting started during the Early Jurassic (ca. 180 Ma) with the sep...
The East African margin between the Somali Basin in the north and the Natal Basin in the south forme...
The rifting of Gondwana started some 180 million years ago. The continental drift created some of th...
The East African margin between the Somali Basin in the north and the Natal Basin in the south forme...
International audienceSeismic reflection and multibeam echosounder data acquired in the Mozambique C...
The offshore branch of the East African Rift System (EARS) has developed during late Cenozoic time a...
Accurate reconstructions of the dispersal of supercontinent blocks are essential for testing contine...
Seismic reflection and multibeam echosounder data were acquired in the Mozambique Channel in 2014 an...
Numerous studies have addressed various aspects of the East African Rift system but surprisingly few...
New seismic reflection, gravity, and magnetic data from offshore East Africa allow the Davie Fractur...
Giant shear processes shaped Africa's southern margin during the break-up of the supercontinent Gond...
Accurate mapping of first-order tectonic features such as oceanic fracture zones and continental mar...
The Gondwana breakup along the Mozambique continental margin caused the formation of extensional and...
Transform continental margins play a major role in plate tectonics. In the last 10 years' petroleum ...
The Davie Ridge is the central morphological element of the Mozambique Channel between East Africa a...
International audienceGondwana splitting started during the Early Jurassic (ca. 180 Ma) with the sep...
The East African margin between the Somali Basin in the north and the Natal Basin in the south forme...
The rifting of Gondwana started some 180 million years ago. The continental drift created some of th...
The East African margin between the Somali Basin in the north and the Natal Basin in the south forme...
International audienceSeismic reflection and multibeam echosounder data acquired in the Mozambique C...
The offshore branch of the East African Rift System (EARS) has developed during late Cenozoic time a...
Accurate reconstructions of the dispersal of supercontinent blocks are essential for testing contine...
Seismic reflection and multibeam echosounder data were acquired in the Mozambique Channel in 2014 an...
Numerous studies have addressed various aspects of the East African Rift system but surprisingly few...
New seismic reflection, gravity, and magnetic data from offshore East Africa allow the Davie Fractur...
Giant shear processes shaped Africa's southern margin during the break-up of the supercontinent Gond...
Accurate mapping of first-order tectonic features such as oceanic fracture zones and continental mar...
The Gondwana breakup along the Mozambique continental margin caused the formation of extensional and...