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- W2143156760 abstract "The Oligo-Aquitanian deposits of the Mula–Pliego basin consist of a marine carbonate platform assemblage (bottom), transitioning into a turbidite wedge (top). This evolution was controlled by tectonics in a piggy-back basin by means of three main mechanisms: first, a flexural tectonic event created the basin; later on, blind-fault-propagation folds deformed it progressively from south to north; finally a tectonic event destroyed the basin. To cite this article: M. Martı́n-Martı́n, A. Martı́n-Algarra, C. R. Geoscience 334 (2002) 363–370. Les dépôts oligo-aquitaniens du bassin de Mula–Pliego débutent par un ensemble carbonaté marin et passent progressivement vers le haut à un « coin » turbiditique ; ils ont été contrôlés par la tectonique, dans un bassin de type transporté (piggy-back). L'évolution tectonique résulte de trois mécanismes principaux : d'abord, une tectonique flexurale, ensuite, une succession de plis de propagation de la déformation du sud vers le nord et, finalement, un ultime événement tectonique, qui détruit le bassin. Pour citer cet article : M. Martı́n-Martı́n, A. Martı́n-Algarra, C. R. Geoscience 334 (2002) 363–370." @default.
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- W2143156760 date "2002-01-01" @default.
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- W2143156760 title "Thrust sequence and syntectonic sedimentation in a piggy-back basin: the Oligo-Aquitanian Mula–Pliego Basin (Internal Betic Zone, SE Spain)" @default.
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- W2143156760 doi "https://doi.org/10.1016/s1631-0713(02)01757-1" @default.
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