A Revised Subduction Inception Model to Explain the Late Cretaceous, Double-Vergent Orogen in the Precollisional Western Tethys: Evidence From the Northern Apennines-Reference-Cited by-同舟云学术

A Revised Subduction Inception Model to Explain the Late Cretaceous, Double-Vergent Orogen in the Precollisional Western Tethys: Evidence From the Northern Apennines

Published:2017-10 Issue:10 Volume:36 Page:2227-2249
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Marroni Michele¹²^ORCID,Meneghini Francesca¹^ORCID,Pandolfi Luca¹²^ORCID

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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