A

Comment on se-2021-7

Abstract

Abstract. The Dinaric Fault System in western Slovenia, consisting of NW–SE-trending, right-lateral strike-slip faults, accommodates the northward motion of Adria with respect to Eurasia. These active faults show a clear imprint in the morphology, and some of them hosted moderate instrumental earthquakes. However, it is largely unknown if the faults also had strong earthquakes in the late Quaternary. This hampers our understanding of the regional tectonics and the seismic hazard. Geological evidence of co-seismic surface ruptures only exists for one historical event, the 1511 Idrija earthquake with a magnitude of ∼ M 6.8, but the causative fault is still disputed. Here we use geomorphological data, near-surface geophysical surveys, and paleoseismological trenching to study two of these faults: the Predjama Fault and the Idrija Fault. In a paleoseismological trench across the Predjama Fault we found deformation features that may have been caused by an earthquake between 13–0.7 ka, very likely not earlier than 8.4 ka. At the Idrija Fault, a surface-rupturing earthquake happened around 2.5 ka. We show that instrumental and historical seismicity data do not capture the strongest events in this area.

Authors 9

  1. Christoph Grà ⁄ tzner corresponding

    Friedrich Schiller University Jena

    Affiliation as printed

    Institute of Geological Sciences, Friedrich-Schiller-Universität Jena, 07749 Jena, Germany

  2. University of Cologne · RWTH Aachen University

    Affiliation as printed

    Neotectonics and Natural Hazards Group, RWTH Aachen University, 52056 Aachen, Germany

    now at: Institute of Geology and Mineralogy, University of Cologne, 50674 Cologne, Germany

  3. Petra Jamšek Rupnik corresponding

    Geological Survey of Slovenia

    Affiliation as printed

    Geological Survey of Slovenia, Ljubljana, 1000, Slovenia

  4. RWTH Aachen University

    Affiliation as printed

    Neotectonics and Natural Hazards Group, RWTH Aachen University, 52056 Aachen, Germany

  5. RWTH Aachen University

    Affiliation as printed

    Neotectonics and Natural Hazards Group, RWTH Aachen University, 52056 Aachen, Germany

  6. BlaÅ ⁄ Vičič corresponding

    The Abdus Salam International Centre for Theoretical Physics (ICTP)

    Affiliation as printed

    The Abdus Salam International Centre for Theoretical Physics, Trieste, 34151, Italy

  7. Marko Vrabec corresponding

    University of Ljubljana

    Affiliation as printed

    Department of Geology, University of Ljubljana, Ljubljana, 1000, Slovenia

  8. Julian Welte corresponding

    Friedrich Schiller University Jena

    Affiliation as printed

    Institute of Geological Sciences, Friedrich-Schiller-Universität Jena, 07749 Jena, Germany

  9. Kamil Ustaszewski corresponding

    Friedrich Schiller University Jena

    Affiliation as printed

    Institute of Geological Sciences, Friedrich-Schiller-Universität Jena, 07749 Jena, Germany

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References 62