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<title lang=en>Determining the present-day kinematics of the Idrija fault (Slovenia) from airborne LiDAR topography</title>
<creator>Moulin, Adrien</creator>
<creator>Benedetti, Lucilla</creator>
<creator>Gosar, Andrej</creator>
<creator>Rupnik, Petra jamsek</creator>
<creator>Rizza, Magali</creator>
<creator>Bourles, Didier</creator>
<creator>Ritz, Jean-François</creator>
<contributor>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Faculty of Natural Sciences and Engineering, Ljubljana</contributor>
<contributor>Geological Survey of Slovenia, Ljubljana</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Earth Observatory of Singapore</contributor>
<contributor>Risques ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 0040-1951</source>
<source>EISSN: 1879-3266</source>
<source>Tectonophysics</source>
<publisher>Elsevier</publisher>
<identifier>hal-01115724</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01115724</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01115724</source>
<source>Tectonophysics, Elsevier, 2014, 628, pp.188-205. 〈10.1016/j.tecto.2014.04.043〉</source>
<identifier>DOI : 10.1016/j.tecto.2014.04.043</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2014.04.043</relation>
<language>en</language>
<subject lang=en>Slip-rate</subject>
<subject lang=en>Fault kinematics</subject>
<subject lang=en>Northern Dinarides</subject>
<subject lang=en>Idrija fault</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Located in central Europe at the junction of the Southern Alps and the Dinarides, the ≈ 100 km long Idrija fault, striking N310 and dipping ≈ 80°NE is often considered as the potential source of the historical 1511 earthquake (estimated macroseismic magnitude: Mm 6.8). Using 1/25,000 to 1/5000 topographical maps, satellite images (SPOT5), 12.5 m illuminated DEM and airborne LiDAR data-derived 1-m-DEM, we examined in detail the Idrija fault trace along a 20-km-long swath in the central portion of the fault. Combining topographic and remote sensing data allows characterizing the recent activity along the Idrija fault and estimating its cumulative displacement along strike.Between Tolmin and Godovič, the fault trace is mostly linear but appears divided into three disconnected segments of 11–20-km-long. Morphological evidences such as offset streams and ridges and major drainage abandonments suggest ongoing movement. At three sites, field observations and LiDAR-DEM analysis allow measuring cumulative dextral offsets comprised between 35 and 65 m. We found two larger offsets of ≈ 140 m and ≈ 360 m at the southeasternmost site. The vertical component is significant and revealed by a rake ranging from 0 to 33°. The derived N303–N310 striking slip-vector is in agreement with the motion along this fault as suggested by the geodesy. Assuming that the smallest measured offsets have been recorded after the last glacial maximum (LGM, about 20 ka ago), the minimum slip-rate for the Idrija fault is about 1.5 mm/yr over this period of time.</description>
<date>2014-07-30</date>
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