Articles | Volume 15, issue 12
https://doi.org/10.5194/se-15-1525-2024
https://doi.org/10.5194/se-15-1525-2024
Research article
 | 
20 Dec 2024
Research article |  | 20 Dec 2024

Reconciling post-orogenic faulting, paleostress evolution, and structural inheritance in the seismogenic northern Apennines (Italy): insights from the Monti Martani Fault System

Riccardo Asti, Selina Bonini, Giulio Viola, and Gianluca Vignaroli

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Cited articles

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Ambrosetti, P., Carboni, M. G., Conti, M. A., Costantini, A., Esu, D., Gandin, A., Girotti, O., Lazzarotto, A., Mazzanti, R., Nicosia, U., Parisi, G., and Sandrelli, F.: Evoluzione paleogeografica e tettonica dei bacini tosco-umbro-laziali nel Pliocene e nel Pleistocene inferiore, Memorie della Società Geologica Italiana, 19, 573–580, 1978. 
Ambrosetti, P., Carboni, M. G., Conti, M. A., Esu, D., Girotti, O., La Monica, G. B., Landini, B., and Parisi, G.: Il Pliocene ed il Pleistocene inferiore del bacino del Fiume Tevere nell'Umbria meridionale: The Pliocene and the Lower Pleistocene of the Tevere Basin in Southern Umbria, Geogr. Fis. Din. Quat., 10, 10–33, 1987a. 
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Short summary
This study addresses the tectonic evolution of the seismogenic Monti Martani Fault System (northern Apennines, Italy). By applying a field-based structural geology approach, we reconstruct the evolution of the stress field and we challenge the current interpretation of the fault system in terms of both geometry and state of activity. We stress that the peculiar behavior of this system during post-orogenic extension is still significantly influenced by the pre-orogenic structural template.
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