Augusto Maresca
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View article: Linking thrust system, back-arc extension, rift inheritance, and crustal delamination in the Tyrrhenian basin–Apennines thrust belt system.
Linking thrust system, back-arc extension, rift inheritance, and crustal delamination in the Tyrrhenian basin–Apennines thrust belt system. Open
In this contribution, we present a kinematic reconstruction for the Tyrrhenian back-arc basin–central Apennines fold-and-thrust belt system during the last 25 Myr, illustrating how its evolution is driven by the interplay between sla…
View article: A crustal balanced-cross section across the central Apennines and the relationship between thick- and thin-skinned tectonics
A crustal balanced-cross section across the central Apennines and the relationship between thick- and thin-skinned tectonics Open
The Apennines form part of the Africa-Eurasia convergent plate boundary and are cored by two diachronous back-arc basins formed in response to slab retreat, separated by the Sardinia-Corsica continental ribbon. Subduction of oceanic lithos…
View article: Rift inheritance in a fold-and-thrust belt evolution: Central Apennine crustal balanced cross-section
Rift inheritance in a fold-and-thrust belt evolution: Central Apennine crustal balanced cross-section Open
The Apennines fold-and-thrust belt builds part of the Africa-Eurasia convergent plate boundary. It developed due to the Neogene subduction of the Alpine Tethys underneath Europe and to the subsequent involvement of the Adria microplate rif…
View article: Timing, Thrusting Mode, and Negative Inversion Along the Circeo Thrust, Apennines, Italy: How the Accretion‐To‐Extension Transition Operated During Slab Rollback
Timing, Thrusting Mode, and Negative Inversion Along the Circeo Thrust, Apennines, Italy: How the Accretion‐To‐Extension Transition Operated During Slab Rollback Open
The evolution of the Apennine wedge has seen the time‐space migration of the forebulge, foredeep, thrust wedge, and back‐arc extension phases in the wake of the Eastward rollback of the subducting Adria slab. In this framework, thrusting a…
View article: A new crustal balanced cross-section through the Central Apennines (Italy)
A new crustal balanced cross-section through the Central Apennines (Italy) Open
The Apennines fold-and-thrust belt, forming part of the Africa-Eurasia plate boundary, developed due to the Neogene subduction of the Alpine Tethys underneath Europe and to the subsequent involvement of the Adria rifted margin into the col…
View article: Post-rift Aptian-Cenomanian extension in Adria, insight from the km-scale Positano-Vico Equense syn-sedimentary fault
Post-rift Aptian-Cenomanian extension in Adria, insight from the km-scale Positano-Vico Equense syn-sedimentary fault Open
During the late Early Cretaceous, at the beginning of the Africa-Europe convergence, some portions of Adria experienced an enigmatic post-rift subsidence acceleration. According to many, this event is likely associated with extensional tec…