Plio-Quaternary transpressive tectonics: a key factor in the structural evolution of the outer Apennine–Adriatic system, Italy

P.P. Pierantoni, J. Chicco, M. Costa and C. Invernizzi
Journal of the Geological Society, 176, 1273-1283, 11 July 2019, https://doi.org/10.1144/jgs2018-199

Article Information

DOI 
https://doi.org/10.1144/jgs2018-199
Published By 
Geological Society of London
Print ISSN 
0016-7649
Online ISSN 
2041-479X
History 
  • Received 10 November 2018
  • Revision received 10 April 2019
  • Accepted 14 April 2019
  • Published 11 July 2019.

Article Versions

Copyright & Usage 
© 2019 The Author(s). Published by The Geological Society of London. All rights reserved

Author Information

  1. P.P. Pierantoni1,
  2. J. Chicco1,
  3. M. Costa2 and
  4. C. Invernizzi1,*
  1. 1School of Science and Technology, Geology Division, University of Camerino, , Via Gentile III da Varano 62032, Camerino, MC, Italy
  2. 2Via Selvelli, , 6, 61032 Fano, Italy
  1. ↵*Correspondence: chiara.invernizzi{at}unicam.it

  • Present address: JC, Department of Earth Sciences, University of Turin, Via Valperga Caluso 35, 10125 Torino, Italy

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Funding

  • Università degli Studi di Camerino

    FAR
    Chiara Invernizzi

  • Università degli Studi di Camerino

    FAR
    Pietro Paolo Pierantoni

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