Polyphase evolution of Pelagonia (northern Greece) revealed by geological and fission-track data

Schenker, F. L.; Fellin, M. G.; Burg, J.-P.

doi:https://doi.org/10.5194/se-6-285-2015

Articles | Volume 6, issue 1

https://doi.org/10.5194/se-6-285-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/se-6-285-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 6, issue 1

Research article

|

25 Feb 2015

Research article |

| 25 Feb 2015

Polyphase evolution of Pelagonia (northern Greece) revealed by geological and fission-track data

F. L. Schenker, M. G. Fellin, and J.-P. Burg

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Final revised paper (published on 25 Feb 2015)
Preprint (discussion started on 10 Nov 2014)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC C1351: 'Comments to the Authors', M. Zattin, 26 Nov 2014
- AC C1392: 'Answer to the comments of M. Zattin published on 26 November 2014', Filippo Luca Schenker, 08 Dec 2014
RC C1364: 'Interactive comment on “Polyphase evolution of Pelagonia (northern Greece) revealed by geological and fission-track data” by F. L. Schenker et al.', Anonymous Referee #2, 01 Dec 2014
- AC C1397: 'Answer to the comments of an Anonymous referee published on 1 December 2014', Filippo Luca Schenker, 08 Dec 2014

Short summary

The eastern Mediterranean is a long-lived seismically active region where the interaction of compressive and extensive tectonics is responsible for complex crustal deformation. The Pelagonian zone in the Hellenides has witnessed such deformational processes since the Mesozoic. This study combines fission-track analysis (recording temperatures <240°C), structural and stratigraphic data that were essential to constrain the polyphase evolution of the Hellenic orogen over 100 Ma.