C
Carlo Doglioni
Researcher at National Institute of Geophysics and Volcanology
Publications - 250
Citations - 12519
Carlo Doglioni is an academic researcher from National Institute of Geophysics and Volcanology. The author has contributed to research in topics: Subduction & Lithosphere. The author has an hindex of 56, co-authored 234 publications receiving 11194 citations. Previous affiliations of Carlo Doglioni include Sapienza University of Rome & University of Florida.
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A proposal for the kinematic modelling of W-dipping subductions - possible applications to the Tyrrhenian-Apennines system
TL;DR: In this article, a frontal wedge is constructed from the stacking of the upper layers of the subducting plate and the syntectonic clastics that fill the foredeep which are progressively involved in thrusting and later by extension.
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On the post-25 Ma geodynamic evolution of the western Mediterranean
TL;DR: Palaeo-reconstruction of the Apenninic arc suggests about 775 km of migration from the Late Oligocene to present along a transect from the Gulf of Lions to Calabria.
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The Puglia uplift (SE Italy): An anomaly in the foreland of the Apenninic subduction due to buckling of a thick continental lithosphere
TL;DR: In this paper, structural signatures comparing the central Adriatic Sea and the Puglia region were found, and the geometry and the kinematics of the frontal accretionary wedge and related foreland changed from that moment on between the two areas.
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Geodynamic evolution of the central and western Mediterranean: Tectonics vs. igneous petrology constraints
TL;DR: In this paper, a geodynamic reconstruction of the Central-Western Mediterranean and neighboring areas during the last 50 million years was presented, including magmatological and tectonic observations.
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Orogens and slabs vs. their direction of subduction
Carlo Doglioni,P. Harabaglia,Saverio Merlini,F. Mongelli,Angelo Peccerillo,Claudia Piromallo +5 more
TL;DR: In this paper, the authors show that the decollement planes behave differently in the two end-members of subduction, i.e., W-directed and E-to-NE-directed subduction zones.