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.
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 ~M6.8, but the causative fault is still disputed. Here we use geomorphological data, near-surface geophysical surveys, and paleoseismological trenching to show that two of these faults, the Predjama Fault and the Idrija Fault ruptured in strong earthquakes in the Holocene. In a paleoseismological trench across the Predjama Fault we found at least one earthquake with a minimum magnitude of MW6.1 that occurred between 13–0.7 ka, very likely not earlier than 8.4 ka. At the Idrija Fault, a surface-rupturing earthquake with a magnitude of at least MW6.1 happened in the last ~2.1 ka. This event could correspond to the 1511 Idrija earthquake. Our results show that the faults rupture in rare, but strong earthquakes, which dominate the seismic moment release. We show that instrumental and historical seismicity data do not capture the strongest events in this area. The fact that many of the NW-SE trending, parallel faults are active implies that the deformation in western Slovenia is distributed, rather than focussed on one major structure.
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