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• W1968728484 abstract "The Gulf of Aden provides an ideal setting to study oblique rifting since numerous structural data are available onshore and offshore. Recent surveys showed that the spatio-temporal evolution of the Gulf of Aden rift system is dominated by three fault orientations: displacement-orthogonal (WSW), rift-parallel (WNW) and an intermediate E–W trend. The oldest parts of the rift that are exposed onshore feature displacement-orthogonal and intermediate directions, whereas the subsequently active necking zone involves mainly rift-parallel faults. The final rift phase recorded at the distal margin is characterised by displacement-orthogonal and intermediate fault orientations. We investigate the evolution of the Gulf of Aden from rift initiation to break-up by means of 3D numerical experiments on lithospheric scale. We apply the finite element model SLIM3D which includes realistic, elasto-visco-plastic rheology and a free surface. Despite recent advances, 3D numerical experiments still require relatively coarse resolution so that individual faults are poorly resolved. We address this issue by proposing a simple post-processing method that uses the surface stress-tensor to evaluate stress regime (extensional, strike-slip, compressional) and preferred fault azimuth. The described method is applicable to any geodynamic model and easy to introduce. Our model reproduces the observed fault pattern of the Gulf of Aden and illustrates how multiple fault directions arise from the interaction of local and far-field tectonic stresses in an evolving rift system. The numerical simulations robustly feature intermediate faults during the initial rift phase, followed by rift-parallel normal faulting at the rift flanks and strike-slip faults in the central part of the rift system. Upon break-up, displacement-orthogonal as well as intermediate faults occur. This study corroborates and extends findings from previous analogue experiments of oblique rifting on lithospheric scale and allows new insights in the timing of fault successions of the Gulf of Aden and continental rifts in general." @default.
• W1968728484 created "2016-06-24" @default.
• W1968728484 creator A5034718981 @default.
• W1968728484 creator A5089281652 @default.
• W1968728484 date "2013-11-01" @default.
• W1968728484 modified "2023-10-02" @default.
• W1968728484 title "The rift to break-up evolution of the Gulf of Aden: Insights from 3D numerical lithospheric-scale modelling" @default.
• W1968728484 cites W1579118674 @default.
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• W1968728484 cites W1629102058 @default.
• W1968728484 cites W1696758048 @default.
• W1968728484 cites W1740076721 @default.
• W1968728484 cites W1778453091 @default.
• W1968728484 cites W1870222434 @default.
• W1968728484 cites W1876892685 @default.
• W1968728484 cites W1968534064 @default.
• W1968728484 cites W1971762715 @default.
• W1968728484 cites W1972739139 @default.
• W1968728484 cites W1973169596 @default.
• W1968728484 cites W1975522343 @default.
• W1968728484 cites W1975777605 @default.
• W1968728484 cites W1976870535 @default.
• W1968728484 cites W1977212386 @default.
• W1968728484 cites W1981225065 @default.
• W1968728484 cites W1983777910 @default.
• W1968728484 cites W1983940963 @default.
• W1968728484 cites W1985807382 @default.
• W1968728484 cites W1986890268 @default.
• W1968728484 cites W1988004226 @default.
• W1968728484 cites W1990236123 @default.
• W1968728484 cites W1990906109 @default.
• W1968728484 cites W1994290480 @default.
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• W1968728484 cites W2005760921 @default.
• W1968728484 cites W2006254584 @default.
• W1968728484 cites W2008014426 @default.
• W1968728484 cites W2022342538 @default.
• W1968728484 cites W2023604624 @default.
• W1968728484 cites W2023781184 @default.
• W1968728484 cites W2024793243 @default.
• W1968728484 cites W2026814260 @default.
• W1968728484 cites W2026982741 @default.
• W1968728484 cites W2030338264 @default.
• W1968728484 cites W2034049221 @default.
• W1968728484 cites W2034896492 @default.
• W1968728484 cites W2039554481 @default.
• W1968728484 cites W2046640225 @default.
• W1968728484 cites W2046876080 @default.
• W1968728484 cites W2051651324 @default.
• W1968728484 cites W2051931229 @default.
• W1968728484 cites W2055127223 @default.
• W1968728484 cites W2055647422 @default.
• W1968728484 cites W2062692849 @default.
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• W1968728484 cites W2071379902 @default.
• W1968728484 cites W2072179830 @default.
• W1968728484 cites W2072358740 @default.
• W1968728484 cites W2075747016 @default.
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• W1968728484 cites W2076833330 @default.
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• W1968728484 cites W2110491183 @default.
• W1968728484 cites W2115980374 @default.
• W1968728484 cites W2125373616 @default.
• W1968728484 cites W2126591790 @default.
• W1968728484 cites W2131270682 @default.
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• W1968728484 cites W2164687304 @default.
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• W1968728484 doi "https://doi.org/10.1016/j.tecto.2013.06.029" @default.
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