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              <p>We conducted a stress ﬁeld analysis of the northern part of the ~700 km long north-southtrending, seismically active Sistan orogenic belt of Eastern Iran formed as a result of the closure of abranch of the Neo-Tethys during the early Cenozoic. Fault kinematic data reveal drastic changes in the stressregime of Eastern Iran during the late Cenozoic, with three successive directions of compression (σ1), from90°N during the middle-late Miocene to 60°N during the late Pliocene and 25°N during the Plio-Quaternary,thereby evidencing a counterclockwise rotation of about 65° of σ1in less than 10 Myr. As shown bycompilation of paleostress data, Plio-Quaternary direction of compression in Sistan coincides with the onerecorded across the whole of Iran and with present-day Arabia-Eurasia convergence direction. This resultsuggests effective stress transfer from the Zagros collision and that Sistan is at present mechanically coupledand shortened along with the rest of the Iranian crust/lithosphere. By contrast, Miocene compression ismarkedly different in the Iranian hinterland (e.g., Sistan, Central Iran, and Kopet Dagh) and in the Zagrosorogen. This could tentatively be related to the end of Sistan collision and/or to the imprint of activedeformation occurring further to the east. The intermediate late Pliocene compression (i.e., 60°N) couldcorrespond to the progressive reorientation of the stress regime, as Sistan gets mechanically coupled to theZagros collision</p>
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