Articles | Volume 13, issue 8
https://doi.org/10.5194/se-13-1327-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-13-1327-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Structural characterization and K–Ar illite dating of reactivated, complex and heterogeneous fault zones: lessons from the Zuccale Fault, Northern Apennines
Dipartimento di Scienze Biologiche, Geologiche ed Ambientali - BiGeA, Università di Bologna, Bologna, Italy
Giovanni Musumeci
Dipartimento di Scienze della Terra, Università di Pisa, Pisa, Italy
Istituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy
Francesco Mazzarini
Istituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy
Lorenzo Tavazzani
Institute of Geochemistry and Petrology, ETH Zürich, 8092
Zürich, Switzerland
Manuel Curzi
Dipartimento di Scienze Biologiche, Geologiche ed Ambientali - BiGeA, Università di Bologna, Bologna, Italy
Espen Torgersen
Geological Survey of Norway, Trondheim, Norway
Roelant van der Lelij
Geological Survey of Norway, Trondheim, Norway
Luca Aldega
Dipartimento di Scienze della Terra, Sapienza Università di
Roma, Rome, Italy
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Cited
13 citations as recorded by crossref.
- High-resolution investigations of fault architecture in space and time L. Del Sole et al. 10.1038/s41598-025-86104-w
- Fracture evaluation of the plutonic basement in the Upper Magdalena Basin: Implications for the development of naturally fractured reservoirs in the Northern Andes M. Rodríguez‐Cuevas et al. 10.1002/gj.4980
- Fluid-rock interaction, skarn genesis, and hydrothermal alteration within an upper crustal fault zone (Island of Elba, Italy) P. Garofalo et al. 10.1016/j.oregeorev.2023.105348
- Dating syn-orogenic exhumation of subducted continental crust: The case of the Northern Apennines F. Giuntoli et al. 10.1016/j.lithos.2024.107801
- Tectonic-Sedimentary evolution of the Tuscan shelf (Italy): Seismic-stratigraphic/structural analysis of Neogenic succession in the Tyrrhenian Sea between Elba Island and Monte Argentario promontory M. Buttinelli et al. 10.1016/j.tecto.2024.230211
- How brittle detachments form and evolve through space and time C. Zuccari et al. 10.1016/j.epsl.2024.119108
- Reconciling post-orogenic faulting, paleostress evolution, and structural inheritance in the seismogenic northern Apennines (Italy): insights from the Monti Martani Fault System R. Asti et al. 10.5194/se-15-1525-2024
- Relative dating of fault activity using the principle of cross-cutting relationships: An automated approach A. Li et al. 10.1016/j.cageo.2024.105702
- Structural architecture and micromechanics of the carbonate-hosted low-angle normal fault, Agri Valley, southern Apennines, Italy R. Novellino et al. 10.1016/j.jsg.2025.105352
- Rifting dismantling an orogenic belt: the interplay between polyphase extensional structures and magmatism in the northern Tyrrhenian Sea (Elba Island, inner Northern Apennines, Italy) A. Brogi et al. 10.1080/00206814.2025.2460032
- Timing, sequence, duration and rate of deformation in fold-and-thrust belts: a review of traditional approaches and recent advances from absolute dating (K–Ar illite/U–Pb calcite) of brittle structures O. Lacombe & N. Beaudoin 10.5802/crgeos.218
- Migration of hot to super-hot palaeo-fluids in an extensional setting (eastern Elba Island, Italy) M. Zucchi et al. 10.1016/j.tecto.2024.230210
- Constraints on upper crustal fluid circulation and seismogenesis from in-situ outcrop quantification of complex fault zone permeability M. Curzi et al. 10.1038/s41598-023-32749-4
13 citations as recorded by crossref.
- High-resolution investigations of fault architecture in space and time L. Del Sole et al. 10.1038/s41598-025-86104-w
- Fracture evaluation of the plutonic basement in the Upper Magdalena Basin: Implications for the development of naturally fractured reservoirs in the Northern Andes M. Rodríguez‐Cuevas et al. 10.1002/gj.4980
- Fluid-rock interaction, skarn genesis, and hydrothermal alteration within an upper crustal fault zone (Island of Elba, Italy) P. Garofalo et al. 10.1016/j.oregeorev.2023.105348
- Dating syn-orogenic exhumation of subducted continental crust: The case of the Northern Apennines F. Giuntoli et al. 10.1016/j.lithos.2024.107801
- Tectonic-Sedimentary evolution of the Tuscan shelf (Italy): Seismic-stratigraphic/structural analysis of Neogenic succession in the Tyrrhenian Sea between Elba Island and Monte Argentario promontory M. Buttinelli et al. 10.1016/j.tecto.2024.230211
- How brittle detachments form and evolve through space and time C. Zuccari et al. 10.1016/j.epsl.2024.119108
- Reconciling post-orogenic faulting, paleostress evolution, and structural inheritance in the seismogenic northern Apennines (Italy): insights from the Monti Martani Fault System R. Asti et al. 10.5194/se-15-1525-2024
- Relative dating of fault activity using the principle of cross-cutting relationships: An automated approach A. Li et al. 10.1016/j.cageo.2024.105702
- Structural architecture and micromechanics of the carbonate-hosted low-angle normal fault, Agri Valley, southern Apennines, Italy R. Novellino et al. 10.1016/j.jsg.2025.105352
- Rifting dismantling an orogenic belt: the interplay between polyphase extensional structures and magmatism in the northern Tyrrhenian Sea (Elba Island, inner Northern Apennines, Italy) A. Brogi et al. 10.1080/00206814.2025.2460032
- Timing, sequence, duration and rate of deformation in fold-and-thrust belts: a review of traditional approaches and recent advances from absolute dating (K–Ar illite/U–Pb calcite) of brittle structures O. Lacombe & N. Beaudoin 10.5802/crgeos.218
- Migration of hot to super-hot palaeo-fluids in an extensional setting (eastern Elba Island, Italy) M. Zucchi et al. 10.1016/j.tecto.2024.230210
- Constraints on upper crustal fluid circulation and seismogenesis from in-situ outcrop quantification of complex fault zone permeability M. Curzi et al. 10.1038/s41598-023-32749-4
Latest update: 11 Mar 2025
Short summary
A structural-geochronological approach helps to unravel the Zuccale Fault's architecture. By mapping its internal structure and dating some of its fault rocks, we constrained a deformation history lasting 20 Myr starting at ca. 22 Ma. Such long activity is recorded by now tightly juxtaposed brittle structural facies, i.e. different types of fault rocks. Our results also have implications on the regional evolution of the northern Apennines, of which the Zuccale Fault is an important structure.
A structural-geochronological approach helps to unravel the Zuccale Fault's architecture. By...