A Revised Subduction Inception Model to Explain the Late Cretaceous, Double-Vergent Orogen in the Precollisional Western Tethys: Evidence From the Northern Apennines
Author:
Affiliation:
1. Dipartimento di Scienze della Terra; Università di Pisa; Pisa Italy
2. Istituto di Geoscienze e Georisorse; CNR; Pisa Italy
Funder
“ATENEO grant” by Pisa University
MIUR PRIN project
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017TC004627/fullpdf
Reference113 articles.
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3. Fragmentation of the Alpine orogenic belt by microplate dispersal;Alvarez;Nature,1974
4. Plate motion and the evolution of Alpine Corsica and Northern Apennine;Argnani;Tectonophysics,2012
5. Late Cretaceous carbonate turbidites of the Northern Apennines: Shaking Adria at the onset of Alpine collision;Argnani;Journal of Geology,2004
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