Journal cover Journal topic
Solid Earth An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 2.380 IF 2.380
  • IF 5-year value: 3.147 IF 5-year
    3.147
  • CiteScore value: 3.06 CiteScore
    3.06
  • SNIP value: 1.335 SNIP 1.335
  • IPP value: 2.81 IPP 2.81
  • SJR value: 0.779 SJR 0.779
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 32 Scimago H
    index 32
  • h5-index value: 31 h5-index 31
Volume 6, issue 1
Solid Earth, 6, 285–302, 2015
https://doi.org/10.5194/se-6-285-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Solid Earth, 6, 285–302, 2015
https://doi.org/10.5194/se-6-285-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

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 et al.
Related authors  
Permeability and seismic velocity anisotropy across a ductile–brittle fault zone in crystalline rock
Quinn C. Wenning, Claudio Madonna, Antoine de Haller, and Jean-Pierre Burg
Solid Earth, 9, 683–698, https://doi.org/10.5194/se-9-683-2018,https://doi.org/10.5194/se-9-683-2018, 2018
Short summary
Related subject area  
Tectonics
Can subduction initiation at a transform fault be spontaneous?
Diane Arcay, Serge Lallemand, Sarah Abecassis, and Fanny Garel
Solid Earth, 11, 37–62, https://doi.org/10.5194/se-11-37-2020,https://doi.org/10.5194/se-11-37-2020, 2020
Short summary
The Geodynamic World Builder: a solution for complex initial conditions in numerical modeling
Menno Fraters, Cedric Thieulot, Arie van den Berg, and Wim Spakman
Solid Earth, 10, 1785–1807, https://doi.org/10.5194/se-10-1785-2019,https://doi.org/10.5194/se-10-1785-2019, 2019
Short summary
From mapped faults to fault-length earthquake magnitude (FLEM): a test on Italy with methodological implications
Fabio Trippetta, Patrizio Petricca, Andrea Billi, Cristiano Collettini, Marco Cuffaro, Anna Maria Lombardi, Davide Scrocca, Giancarlo Ventura, Andrea Morgante, and Carlo Doglioni
Solid Earth, 10, 1555–1579, https://doi.org/10.5194/se-10-1555-2019,https://doi.org/10.5194/se-10-1555-2019, 2019
Short summary
Lithosphere tearing along STEP faults and synkinematic formation of lherzolite and wehrlite in the shallow subcontinental mantle
Károly Hidas, Carlos J. Garrido, Guillermo Booth-Rea, Claudio Marchesi, Jean-Louis Bodinier, Jean-Marie Dautria, Amina Louni-Hacini, and Abla Azzouni-Sekkal
Solid Earth, 10, 1099–1121, https://doi.org/10.5194/se-10-1099-2019,https://doi.org/10.5194/se-10-1099-2019, 2019
Short summary
A systematic comparison of experimental set-ups for modelling extensional tectonics
Frank Zwaan, Guido Schreurs, and Susanne J. H. Buiter
Solid Earth, 10, 1063–1097, https://doi.org/10.5194/se-10-1063-2019,https://doi.org/10.5194/se-10-1063-2019, 2019
Short summary
Cited articles  
Anders, B., Reischmann, T., and Kostopoulos, D.: Zircon geochronology of basement rocks from the Pelagonian Zone, Greece: constraints on the pre-Alpine evolution of the westernmost Internal Hellenides, Internat. J. Earth Sci., 96, 639–661, 2007.
Aubouin, J.: Des tectoniques superposées et de leur signification par rapport aux modèles géophysiques: l'example des Dinarides; paléotectonique, tectonique, tarditectonique, néotectonique Bull. Soc. Géol. Fr., 7, 428–460, 1973.
Baumgartner, P. O.: Jurassic sedimentary evolution and nappe emplacement in the Argolis Peninsula (Peloponnesus; Greece), Mém. Soc. Helv. Sci. Nat., 99, 1–111, 1985.
Bernoulli, D. and Laubscher, H.: The palinspastic problem of the Hellenides, Ecl. Geol. Helvet., 65, 1007–1118, 1972.
Bortolotti, V., Carras, N., Chiari, M., Fazzuoli, M., Marcucci, M., Photiades, A., and Principi, G.: The Argolis Peninsula in the palaeogeographic and geodynamic frame of the Hellenides, Ofioliti, 28, 79–94, 2003.
Publications Copernicus
Download
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.
The eastern Mediterranean is a long-lived seismically active region where the interaction of...
Citation