3‐D Architecture and Plio‐Quaternary Evolution of the Paola Basin: Insights Into the Forearc of the Tyrrhenian‐Ionian Subduction System-Reference-Cited by-同舟云学术

3‐D Architecture and Plio‐Quaternary Evolution of the Paola Basin: Insights Into the Forearc of the Tyrrhenian‐Ionian Subduction System

Author:

Corradino M.¹^ORCID,Pepe F.¹^ORCID,Bertotti G.²^ORCID,Picotti V.³^ORCID,Monaco C.⁴⁵^ORCID,Nicolich R.⁶^ORCID

Affiliation:

1. Dipartimento di Scienze della Terra e del Mare University of Palermo Palermo Italy

2. Faculty of Civil Engineering and Geosciences Delft University of Technology Delft Netherlands

3. Department of Earth Sciences Geological Institute, ETH Zurich Zürich Switzerland

4. Dipartimento di Scienze Biologiche, Geologiche e Ambientali University of Catania Catania Italy

5. CRUST‐Centro inteRUniversitario per l'analisi SismoTettonica tridimensionale con applicazioni territoriali Chieti Italy

6. Istituto Nazionale di Oceanografia e Geofisica Sperimentale Trieste Italy

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

Reference127 articles.

1. L'arco calabro‐peloritano nell'orogene appenninico‐maghrebide;Amodio‐Morelli L.;Memorie Della Societa'Geologica Italiana,1976

3. Paola slope basin: Evidence of regional contraction on the eastern Tyrrhenian margin;Argnani A.;Memorie Della Società Geologica Italiana,1988

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