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Renato Funiciello

Researcher at Roma Tre University

Publications -  157
Citations -  6191

Renato Funiciello is an academic researcher from Roma Tre University. The author has contributed to research in topics: Volcano & Fault (geology). The author has an hindex of 42, co-authored 157 publications receiving 5794 citations. Previous affiliations of Renato Funiciello include Sapienza University of Rome & Leonardo.

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Midcrustal shear zones in postorogenic extension: Example from the northern Tyrrhenian Sea

TL;DR: In this article, a model for ductile extension and metamorphic evolution in the northern Tyrrhenian Sea from Alpine Corsica to Tuscany is presented. But the model involves retreat of the slab and migration of the volcanic arc.
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Interactions between mantle upwelling, drainage evolution and active normal faulting: an example from the central Apennines (Italy)

TL;DR: In this paper, the authors show that the processes that have shaped the Quaternary surface development of the Apennines in central Italy are all consequences of a single subcrustal process, the upwelling of the mantle.
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The dynamics of back‐arc extension: an experimental approach to the opening of the Tyrrhenian Sea

TL;DR: In this paper, the authors used 3D laboratory experiments to simulate a retreating subduction process in a compressional regime oriented perpendicularly to the direction of subduction, in which they also tested the influence of the gravitational collapse of the overriding plate.
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Styles of back-arc extension in the Central Mediterranean

TL;DR: In the Central Mediterranean two back-arc basins, the Liguro-Provencal (LPb) and the Tyrrhenian basin (Tb), opened progressively and consecutively from the late Eocene-Oligocene to the present as discussed by the authors.
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Magnetic fabric of weakly deformed clay-rich sediments in the italian peninsula : relationship with compressional and extensional tectonics

TL;DR: In this paper, the results of anisotropy of magnetic susceptibility (AMS) analyses carried out in weakly deformed Neogene and Quaternary clay-rich sediments from different compressional and extensional settings of the Italian peninsula were discussed.