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- W1998584923 abstract "The Borbera Valley (northwestern Italy) is located in a complex geological area where the linkage between Alps and Apennines occurs. In this area the Antola Unit (Late Cretaceous–Palaeocene) is unconformably overlain by the Upper Eocene–Miocene succession of the Tertiary Piedmont Basin. The structural analysis indicates the occurrence of a folding phase of Late Oligocene–Early Miocene age, characterised by recumbent F2 folds. These folds are superposed onto D1 structures related to an early folding phase of Middle Eocene, affecting only the Antola Unit. The occurrence of map-scale D2 folding phase structures that affect the Tertiary Piedmont Basin succession suggests that the linkage area between Alps and Apennines was reactivated during the Late Oligocene–Early Miocene. To cite this article: M. Marroni et al., C. R. Geoscience 334 (2002) 565–572. La vallée de la Borbera (Italie nord-occidentale) est située au sein d'une zone géologiquement compliquée, où sont visibles les rapports Alpes–Apennins. Dans cette zone, l'unité Antola (Crétacé supérieur–Paléocène) est surmontée, en discordance, par la succession du Bassin tertiaire piémontais (Éocène supérieur à Miocène). Les analyses structurales indiquent la présence d'une phase de plissement (Oligocène supérieur–Miocène inférieur), caractérisée par des plis renversés F2. Ces plis se superposent à des structures D1, plus anciennes, relatives à une phase de plissement de l'Éocène moyen, qui intéressent uniquement l'unité Antola. La présence d'une phase de plissement D2 à l'échelle cartographique, qui implique la succession sédimentaire du Bassin tertiaire piémontais, suggère donc que les rapports entre Alpes et Apennins ont été repris durant l'Oligocène supérieur–Miocène inférieur. Pour citer cet article : M. Marroni et al., C. R. Geoscience 334 (2002) 565–572." @default.
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- W1998584923 date "2002-01-01" @default.
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- W1998584923 title "Polyphase folding at upper structural levels in the Borbera Valley (northern Apennines, Italy): implications for the tectonic evolution of the linkage area between Alps and Apennines" @default.
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- W1998584923 doi "https://doi.org/10.1016/s1631-0713(02)01784-4" @default.
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