Search Results - "Dauteuil, O."

Highly Contrasted Geochemical Pattern in Sediments of the Okavango Delta, Botswana Driven by Dust Supply, Hydrological Heritage and Biogeochemical Reactions by Jolivet, M., Dauteuil, O., Dia, A., Davranche, M., Pierson‐Wickmann, A.‐C., Barrier, L., Murray‐Hudson, M., Mazrui, Nashaat, Marsac, R., Cheng, Feng, Li, Xiangzhong

“…The Okavango Delta in North Botswana is a hot‐spot of biodiversity within the semi‐arid central part of the South African plateau. This endorheic ecosystem is…”
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Trace Metal Enrichments in Water of the Okavango Delta (Botswana): Hydrological Consequences by O. Dauteuil, M. Jolivet, A. Dia, M. Murray‐Hudson, K. Makati, L. Barrier, M. Bouhnik Le Coz, A. Audran, A. Radenac

“…Abstract The Okavango Delta in northern Botswana is an endorheic ecosystem formed by 150,000 islands surrounded by a flood plain. The vegetation of these…”
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Reply to Comment by Terence McCarthy and Marc Humphries on “Highly Contrasted Geochemical Pattern in Sediments of the Okavango Delta, Botswana Driven by Dust Supply, Hydrological Heritage and Biogeochemical Reactions” by Jolivet, M., Dauteuil, O., Dia, A., Davranche, M., Pierson‐Wickmann, A.‐C., Barrier, L., Murray‐Hudson, M., Mazrui, N., Marsac, R., Cheng, Feng, Li, Xiangzhong

“…In southern Africa, the Okavango Delta is a large alluvial fan sustaining a unique wetlands ecosystem in the heart of the Kalahari desert. The Delta is fed by…”
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Long-term stratigraphic evolution of Atlantic-type passive margins: A numerical approach of interactions between surface processes, flexural isostasy and 3D thermal subsidence by Rouby, D., Braun, J., Robin, C., Dauteuil, O., Deschamps, F.

“…The thermal and flexural evolution of passive margins is impacted by the (un)loading effects of erosion/sedimentation processes, which, in turn, affect their…”
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Rheological-layered basin under strike-slip deformation: analogue approach at crustal scale by Dauteuil, O., Homberg, C., Rocher, M., Amarouche, M., Kermarrec, J. J., Jegat, Y.

“…In sedimentary basins, sediment type and deposit and burial conditions generate successive layers with various rheologies reacting differently to boundary…”
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Variations in amount and direction of seafloor spreading along the northeast Atlantic Ocean and resulting deformation of the continental margin of northwest Europe by Le Breton, E., Cobbold, P. R., Dauteuil, O., Lewis, G.

“…The NE Atlantic Ocean opened progressively between Greenland and NW Europe during the Cenozoic. Seafloor spreading occurred along three ridge systems: the…”
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Sediment supply to the Orange sedimentary system over the last 150 My: An evaluation from sedimentation/denudation balance by Rouby, D., Bonnet, S., Guillocheau, F., Gallagher, K., Robin, C., Biancotto, F., Dauteuil, O., Braun, J.

“…The South African plateau is bordered by passive margin basins preserving the terrigeneous sediment produced during onshore erosion. As such, these basins…”
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Post-breakup evolution of the Namibian margin: Constraints from numerical modeling by Dauteuil, O., Rouby, D., Braun, J., Guillocheau, F., Deschamps, F.

“…The Namibian margin evolution started 130Myr ago after the breakup between South America and southern Africa. Today, it shows specific features: (i) an…”
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Post-glacial rebound of Iceland during the Holocene by Le Breton, Eline, Dauteuil, O, Biessy, G

“…The geodynamic context of Iceland provides the rare opportunity to analyse the combined effects of a ridge and a hotspot on deformation processes. From a…”
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Propagation of an oblique spreading centre: the western Gulf of Aden by Dauteuil, O., Huchon, P., Quemeneur, F., Souriot, T.

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Fast and partitioned postglacial rebound of southwestern Iceland by Biessy, G., Dauteuil, O., Van Vliet‐Lanoë, B., Wayolle, A.

“…Located both on the Mid‐Atlantic Ridge and above a mantle plume, Iceland is subject to horizontal and vertical motions. Many studies described these…”
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Lithosphere strength controls oceanic transform zone structure: insights from analogue models by Dauteuil, O., Bourgeois, O., Mauduit, T.

“…Summary Oceanic transform zones have often been regarded as plate boundaries. The origin of their structural variability is poorly constrained. A simple…”
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Geoelectrical Tomography Investigating and Modeling of Fractures Network around Bittit Spring (Middle Atlas, Morocco) by Qarqori, Kh, Rouai, M., Moreau, F., Saracco, G., Dauteuil, O., Hermitte, D., Boualoul, M., Le Carlier de Veslud, C.

“…Direct current Resistivity (DCR) method was carried out to characterize the hydrogeological connection between the Tabular Middle Atlas (TMA) and the Saïs…”
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Deformation partitioning inside a fissure swarm of the northern Icelandic rift by Dauteuil, O., Angelier, J., Bergerat, F., Verrier, S., Villemin, T.

“…Extension in an oceanic rift domain is accommodated by fissuring and faulting processes. The fissuring, including dike injection, involves extension and an…”
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Sediment supply to the Orange sedimentary system over the last 150My: An evaluation from sedimentation/denudation balance by Rouby, D, Bonnet, S, Guillocheau, F, Gallagher, K, Robin, C, Biancotto, F, Dauteuil, O, Braun, J

“…The South African plateau is bordered by passive margin basins preserving the terrigeneous sediment produced during onshore erosion. As such, these basins…”
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Interactions between magmatism and tectonics in Iceland: a review by Dauteuil, O., Bergerat, F.

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Analogue modeling of faulting pattern, ductile deformation, and vertical motion in strike-slip fault zones by Dauteuil, O., Mart, Y.

“…The relationship between faulting, ductile deformation, and vertical displacement in provinces of strike‐slip faults were analyzed using analogue modeling. The…”
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Holocene vertical deformation outside the active rift zone of north Iceland by Dauteuil, O., Bouffette, J., Tournat, F., Van Vliet-Lanoë, B., Embry, J.C., Quété, Y.

“…In Iceland, the main deformation activity occurs not only in the active rift zone where volcanism and seismicity coexist in fissure swarms but also in the…”
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Deformation partitioning in a slow spreading ridge undergoing oblique extension: Mohns Ridge, Norwegian Sea by Dauteuil, O., Brun, J.‐P.

“…Although oceanic spreading is often perpendicular to the ridge trends, in some cases the angle between these two directions can be significantly less than 90°…”
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Cenozoic deformation of the South African plateau, Namibia: Insights from planation surfaces by Picart, C., Dauteuil, O., Pickford, M., Owono, F. Mvondo

“…[Display omitted] •Bulging affected the South African plateau during the Oligocene.•Planation surfaces are markers of short and long wavelength deformation…”
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