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        <identifier>oai:figshare.com:article/34054314</identifier>
        <datestamp>2026-10-02T05:33:21Z</datestamp>
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          <dc:title>Data Sheet 1_Imaging the shear deformation zone along the Kefalonia transform fault zone.docx</dc:title>
          <dc:creator>V. Anagnostou (25162359)</dc:creator>
          <dc:creator>E. Papadimitriou (25162362)</dc:creator>
          <dc:creator>V. Karakostas (11497870)</dc:creator>
          <dc:subject>Solid Earth Sciences</dc:subject>
          <dc:subject>Kefalonia fault</dc:subject>
          <dc:subject>Kefalonia transform fault zone</dc:subject>
          <dc:subject>KTFZ</dc:subject>
          <dc:subject>Lefkada fault</dc:subject>
          <dc:subject>principal component analysis</dc:subject>
          <dc:subject>relocated seismicity</dc:subject>
          <dc:subject>shear deformation zone</dc:subject>
          <dc:description>&lt;p&gt;We quantify the three-dimensional geometry and the across-fault width of the seismically active shear deformation zone of the segments ruptured by large (M &gt; 6.0) strike-slip main shocks of the Kefalonia Transform Fault Zone (KTFZ), the 2014 Kefalonia doublet and the 2015 Lefkada earthquake. Using high-resolution relocated aftershock seismicity for these sequences (1154 earthquakes, M 1.4–6.1, and 1291 earthquakes, M 0.2–6.5, respectively) and following the approach of Perrin et al. (2021), we estimate local best-fitting fault planes in moving windows along strike using principal component analysis (PCA), measure hypocentral distances orthogonal to each plane, and stack the normalized fault-normal distance profiles to determine the characteristic inner and outer bounds of the active shear zone (W&lt;sub&gt;S1&lt;/sub&gt; and W&lt;sub&gt;S2&lt;/sub&gt;). A regularized power-law function is fitted to the stacked distribution, marking W&lt;sub&gt;S1&lt;/sub&gt; at the distance of maximum curvature, and W&lt;sub&gt;S2&lt;/sub&gt; at the distance where the distribution departs from the power law. The two sequences yield W&lt;sub&gt;S1&lt;/sub&gt; values of 0.83 km for the Kefalonia and 0.50 km for the Lefkada sequences and W&lt;sub&gt;S2&lt;/sub&gt; values of 1.88 km and 1.49 km, respectively. Assuming approximate symmetry around the local best-fitting plane, these correspond to full active shear-zone widths of about 3.8 and 3.0 km, respectively. Map-view traces of the local PCA-derived fault patches reveal coherent principal fault orientations together with oblique secondary alignments. These orientations are consistent with earlier interpretations of a segmented dextral transform zone containing relay and transfer structures. The results provide a reproducible, seismicity-based framework for characterizing active shear-zone width, segmentation, and secondary-fault activation along the most seismically hazardous strike-slip system in the eastern Mediterranean.&lt;/p&gt;</dc:description>
          <dc:date>2026-10-02T05:33:21Z</dc:date>
          <dc:type>Dataset</dc:type>
          <dc:type>Dataset</dc:type>
          <dc:identifier>10.3389/feart.2026.1939552.s001</dc:identifier>
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          <dc:rights>CC BY 4.0</dc:rights>
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