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Published in 2020 at "Earth-Science Reviews"
DOI: 10.1016/j.earscirev.2020.103136
Abstract: Abstract Deepwater fold-thrust belts (FTBs) are predominantly formed by the deformation of sedimentary sequences as a result of subduction of oceanic plates at active margins, gravitational failure at passive margins, or a combination of these…
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Keywords:
gravity driven;
fold thrust;
plate convergence;
convergence ... See more keywords