9 documents found, page 1 of 1
From the lebombo monocline to the Mozambique deep basin, using combined wide-an...
Moulin, Maryline; Leprêtre, Angelique; Verrier, Fanny; Schnürle, Philippe; Evain, Mikael; Clarens, Philippe; Thompson, Joseph; Dias, NunoThe North Natal valley (NNV), South Mozambique margin, is a key area for the understanding of the SW Indian Ocean history since the Gondwana break-up as its crustal nature and geometry strongly impacted the recon-struction of the paleogeography before the rifting. It is also of considerable importance for the understanding of the evolution of a margin system as the NNV is situated at the transition between dive...
Deep structure of the Pará-Maranhão/Barreirinhas passive margin in the equatori...
Aslanian, Daniel; Gallais, Flora; Afilhado, Alexandra; Schnurle, Philippe; Moulin, Maryline; Evain, Mikael; Dias, Nuno; Soares, José; Fuck, ReinhartThe Pará-Maranhão/Barreirinhas margin, North Brazil, is a pull-apart passive margin, with two strike-slip borders, formed during the opening of the Equatorial Atlantic Ocean during Cretaceous time. Its geometry and evolution are speculative due to the lack of information on the crustal structure and the crustal nature. We present here the E-W profiles of the MAGIC (Margins of brAzil, Ghana and Ivory Coast) deep...
Imaging early oceanic crust spreading in the Equatorial Atlantic Ocean: insight...
Moulin, Maryline; Schnurle, Philippe; Afilhado, Alexandra; Gallais, Flora; Dias, Nuno; Evain, Mikael; Soares, José; Fuck, ReinhardtDuring the MAGIC (Margins of brAzil, Ghana, and Ivory Coast) experiment, five combined wide-angle, and reflection seismic profiles were acquired in the Pará-Maranhão/Barreirinhas/Ceará basins northern Brazil. This is a pull-apart passive margin, with two strike-slip borders. The equipment deployed includes 143 sea-bottom seismometers (OBS), a 4.5-km seismic streamer, and a 7587-in3 airgun array. In this paper, ...
The limpopo magma-rich transform margin, south Mozambique: 1. Insights from dee...
Watremez, L.; LEROY, Sylvie; D'Acremont, Elia; Roche, Vincent; Evain, Mikael; Lepretre, A.; Verrier, F.; Aslanian, Daniel; Dias, NunoA variety of structures results from the interplay of evolving far-field forces, plate kinematics, and magmatic activity during continental break-up. The east Limpopo transform margin, offshore northern Mozambique, formed as Africa and Antarctica separated during the mid-Jurassic period break-up of the Gondwana supercontinent. The nature of the crust onshore has been discussed for decades in an effort to resolv...
Gondwana breakup: messages from the North Natal Valley
Moulin, Maryline; Aslanian, Daniel; Evain, Mikael; Lepretre, Angelique; Schnurle, Philippe; Verrier, Fanny; Thompson, Joseph; De Clarens, PhilippeThe Natal Valley, offshore Mozambique, is a key area for understanding the evolution of East Gondwana. Within the scope of the integrated multidisciplinary PAMELA project, we present new wide-angle seismic data and interpretations, which considerably alter Geoscience paradigms. These data reveal the presence of a 30-km-thick crust that we argue to be of continental nature. This falsifies all the most recent pal...
Monte Carlo approach to assess the uncertainty of wide-angle layered models: Ap...
Loureiro, Afonso; Afilhado, Alexandra; Matias, Luis; Moulin, Maryline; Aslanian, DanielIn the Santos Basin (Brazil), two parallel wide-angle refraction profiles show different crustal structures. One shows moderate crustal velocity gradient, and a clear Moho with topography. The other has an anomalous velocity zone, and no clear Moho reflections. This has large implications on the geological and geodynamical interpretation of the basin. Model uncertainties must be excluded as a source of t hese d...
Deep structure of the Santos basin-São Paulo plateau system, SE Brazil
Evain, M.; Afilhado, Alexandra; Rigoti, C.; Loureiro, A.; Alves, D.; Klingelhoefer, Frauke; Schnurle, Philippe; Feld, Aurelie; Fuck, R; Soares, J.The structure and nature of the crust underlying the Santos Basin-São Paulo Plateau System (SSPS), in the SE Brazilian margin, are discussed based on five wide-angle seismic profiles acquired during the Santos Basin (SanBa) experiment in 2011. Velocity models allow us to precisely divide the SSPS in six domains from unthinned continental crust (Domain CC) to normal oceanic crust (Domain OC). A seventh domain (D...
Deep crustal structure across a young passive margin from wide-angle and reflec...
Moulin, Maryline; Klingelhoefer, Frauke; Afilhado, Alexandra; Aslanian, Daniel; Schnurle, Philippe; Nouze, Herve; Rabineau, Marina; Beslier, Marie-OdileThe conjugate margins system of the Gulf of Lion and West Sardinia (GLWS) represents a unique natural laboratory for addressing fundamental questions about rifting due to its landlocked situation, its youth, its thick sedimentary layers, including prominent palaeo-marker such as the MSC event, and the amount of available data and multidisciplinary studies. The main goals of the SARDINIA experiment, were to (i) ...
Deep crustal structure across a young passive margin from wide-angle and reflec...
Afilhado, Alexandra; Moulin, Maryline; Aslanian, Daniel; Schnurle, Philippe; Klingelhoefer, Frauke; Nouze, Herve; Rabineau, Marina; Leroux, EstelleGeophysical data acquired on the conjugate margins system of the Gulf of Lion and West Sardinia (GLWS) is unique in its ability to address fundamental questions about rifting (i.e. crustal thinning, the nature of the continent-ocean transition zone, the style of rifting and subsequent evolution, and the connection between deep and surface processes). While the Gulf of Lion (GoL) was the site of several deep sei...