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Seismic evidence for plume-derived volcanism during formation of the continental margin in southern Davis Strait and northern Labrador Sea ArchiMer
Gerlings, Joanna; Funck, Thomas; Jackson, H. Ruth; Louden, Keith E.; Klingerhoefer, Frauke.
The crustal structure in the southern Davis Strait and the adjacent ocean-continent transition zone in NE Labrador Sea was determined along a 185-km-long refraction/wide-angle reflection seismic transect to study the impact of the Iceland mantle plume to this region. A P-wave velocity model was developed from forward and inverse modelling of dense airgun shots recorded by ocean bottom seismographs. A coincident industry multichannel reflection seismic profile was used to guide the modelling as reflectivity could be identified down to Moho. The model displays a marked lateral change of velocity structure. The sedimentary cover (velocities 1.8-3.9 km s(-1)) is up to 4 km thick in the north and thins to 1 km in the south. The segment of the line within...
Tipo: Text Palavras-chave: Crustal structure; Hotspots; Continental margins: transform; Continental margins: divergent.
Ano: 2009 URL: http://archimer.ifremer.fr/doc/2009/publication-6848.pdf
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Geophysical evidence for a transform margin offshore Western Algeria: a witness of a subduction-transform edge propagator? ArchiMer
Badji, Rabia; Charvis, Philippe; Bracene, Rabah; Galve, Audrey; Badsi, Madjid; Ribodetti, Alessandra; Benaissa, Zahia; Klingelhoefer, Frauke; Medaouri, Mourad; Beslier, Marie-odile.
For the first time, a deep seismic data set acquired in the frame of the Algerian-French SPIRAL program provides new insights regarding the origin of the westernmost Algerian margin and basin. We performed a tomographic inversion of traveltimes along a 100-km-long wide-angle seismic profile shot over 40 ocean bottom seismometers offshore Mostaganem (Northwestern Algeria). The resulting velocity model and multichannel seismic reflection profiles show a thin (3-4 km thick) oceanic crust. The narrow ocean-continent transition (less than 10 km wide) is bounded by vertical faults and surmounted by a narrow almost continuous basin filled with Miocene to Quaternary sediments. This fault system, as well as the faults organized in a negative-flower structure on the...
Tipo: Text Palavras-chave: Seismic tomography; Continental margins: transform; Crustal structure; Africa; Europe..
Ano: 2015 URL: http://archimer.ifremer.fr/doc/00255/36670/35278.pdf
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