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2022
DOI: 10.1002/essoar.10510709.1
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Analogue models of lithospheric-scale rifting monitored in an X-ray CT scanner

Abstract: Rifting and the formation of rifted margins during continental break-up represent a fundamental part of the Wilson cycle (e.g., Wilson, 1966;Wilson et al., 2019). The dynamic evolution of rifts and rifted margins and the processes involved is intensely studied for various reasons. Not only do rifts and rifted margins harbor vast fossil energy reserves (

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References 102 publications
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