The NW-SE trending Northern Apennine Mountains consist of a series of allochthonous units which were thrust generally to the NE during Neogene crustal shortening, in the direction of a foreland basin to the east and NE. On the hinterland (internal) side of this fold-and-thrust belt, a series of small-scale sedimentary basins developed from the late Miocene and were deformed at the same time. The late Tortonian-Pleistocene evolution of the Northern Apennines has previously been considered by most authors in terms of a classical model of a NE-migrating compressional front, which was followed in time and space by a hinterland extensional regime related to the development of the Tyrrhenian Basin. This paper presents new structural data from both the external parts of the Northern Apennines and the late Tortonian-Pleistocene basins located in the internal sector. In the Northern Apennine thrust belt, reactivation and out-of-sequence geometries for the thrust faults have been recorded.

Compressive Neogene-Quaternary tectonics in the hinterland area of the Northern Apennines. Constraints for a general evolutive reinterpretation / M. BOCCALETTI; M. BONINI; G. MORATTI; F. SANI. - In: JOURNAL OF PETROLEUM GEOLOGY. - ISSN 0141-6421. - STAMPA. - 22:(1999), pp. 37-60.

Compressive Neogene-Quaternary tectonics in the hinterland area of the Northern Apennines. Constraints for a general evolutive reinterpretation.

SANI, FEDERICO
1999

Abstract

The NW-SE trending Northern Apennine Mountains consist of a series of allochthonous units which were thrust generally to the NE during Neogene crustal shortening, in the direction of a foreland basin to the east and NE. On the hinterland (internal) side of this fold-and-thrust belt, a series of small-scale sedimentary basins developed from the late Miocene and were deformed at the same time. The late Tortonian-Pleistocene evolution of the Northern Apennines has previously been considered by most authors in terms of a classical model of a NE-migrating compressional front, which was followed in time and space by a hinterland extensional regime related to the development of the Tyrrhenian Basin. This paper presents new structural data from both the external parts of the Northern Apennines and the late Tortonian-Pleistocene basins located in the internal sector. In the Northern Apennine thrust belt, reactivation and out-of-sequence geometries for the thrust faults have been recorded.
1999
22
37
60
M. BOCCALETTI; M. BONINI; G. MORATTI; F. SANI
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Utilizza questo identificatore per citare o creare un link a questa risorsa: https://hdl.handle.net/2158/223080
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