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        <datestamp>2026-09-25T08:44:54Z</datestamp>
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          <dc:title>Testing the rigid block rotation model in Central-Eastern Iran under active tectonic regime</dc:title>
          <dc:creator>Ahad Nouri (18008157)</dc:creator>
          <dc:creator>Behnam Rahimi (18008160)</dc:creator>
          <dc:creator>Václav Vavryčuk (5067011)</dc:creator>
          <dc:subject>Biophysics</dc:subject>
          <dc:subject>Neuroscience</dc:subject>
          <dc:subject>Environmental Sciences not elsewhere classified</dc:subject>
          <dc:subject>Chemical Sciences not elsewhere classified</dc:subject>
          <dc:subject>Biological Sciences not elsewhere classified</dc:subject>
          <dc:subject>Cancer</dc:subject>
          <dc:subject>Central-Eastern Iran</dc:subject>
          <dc:subject>block rotation</dc:subject>
          <dc:subject>focal mechanism</dc:subject>
          <dc:subject>maximum horizontal stress</dc:subject>
          <dc:subject>strike-slip fault</dc:subject>
          <dc:description>&lt;p&gt;Central-Eastern Iran (CEI) is a strike-slip zone comprising two sets of right-lateral fault zones arranged in NNW-SSE and N-S directions. This configuration provides an opportunity to test the block rotation model within a natural strike-slip fault zone. Therefore, in this study, we apply a fault-bounded block rotation model, developed for strike-slip zones, to evaluate the compatibility of this model with the kinematics of the CEI since the Neogene. The cumulative offsets and slip rates along the block-bounding faults predicted by this model are consistent with those estimated from geological, geomorphological, and geodetic studies, at least within their uncertainties. The results show that the CEI accommodates Arabian-Eurasian convergence primarily through strike-slip faulting. Furthermore, rotation of fault-bounded blocks in the CEI can accommodate part of the convergence, while also exerting a significant influence on the structural geometry and seismicity of the region. Integrating the results of the fault-bonded block rotation model with stress analysis shows that both the orientation of the maximum horizontal compressive stress (&lt;i&gt;S&lt;/i&gt;&lt;sub&gt;&lt;i&gt;Hmax&lt;/i&gt;&lt;/sub&gt;) relative to the fault strike and the rotation of fault-bounded blocks control the sense of shear on faults in CEI. This study may help explain how large strike-slip faults can control the structural framework of a region through rotation of fault-bounded blocks.&lt;/p&gt;</dc:description>
          <dc:date>2026-09-25T08:44:54Z</dc:date>
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          <dc:identifier>10.6084/m9.figshare.33994123.v1</dc:identifier>
          <dc:relation>https://figshare.com/articles/dataset/Testing_the_rigid_block_rotation_model_in_Central-Eastern_Iran_under_active_tectonic_regime/33994123</dc:relation>
          <dc:rights>CC BY 4.0</dc:rights>
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