The 2019–2020 Khalili (Iran) Earthquake Sequence— Anthropogenic Seismicity in the Zagros Simply Folded Belt?

This work was supported by the International Training Course "Seismology and Seismic Hazard Assessment,'' which has been funded by the GeoForschungsZentrum Potsdam (GFZ) and the German Federal Foreign Office through the German Humanitarian Assistance program, grant S08‐60 321.50 ALL 03/19. Furthermore, M. Jamalreyhani acknowledges support by a grant from the Iran National Science Foundation (INSF) under a research project “97013349.” E. Nissen was supported by the Natural Sciences and Engineering Research Council of Canada through Discovery Grant 2017‐04029, the Canada Foundation for Innovation, the British Columbia Knowledge Development Fund, and a Tier 2 Canada Research Chair. J. A. López‐Comino has also received funding from the European Union's Horizon 2020 research and innovation program under the Marie Skłodowska‐Curie grant agreement 754446 and UGR Research and Knowledge Transfer Found–Athenea3i and by project 407141557 of the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation). Most of the maps were prepared using the Pyrocko toolbox and GMT 5 software. We are grateful to all data research centers and networks for providing the data used in this study. InSAR interferograms were made using freely available Copernicus Sentinel data (2017; https://scihub.copernicus.eu/ ). We are thankful to Gudrun Richter, Christian Heberland, Sebastian Hainzl, Torsten Dahm, and Mir Ali Hassanzadeh for constructive comments on this work. M. Jamalreyhani and P. Büyükakpınar are very grateful to Claus Milkereit and Dorina Kroll for supporting them, during their visit to the GFZ Potsdam. Furthermore, we are grateful to Editor Rachel Abercrombie, the associate editor, and four anonymous reviewers for their valuable comments and suggestions that helped us to improve the manuscript. ; The seismic catalog and waveforms of the Iran network were downloaded from the Iranian Seismological Center (IRSC) available at http://irsc.ut.ac.ir/ . The IRSC waveforms are freely available for the events with magnitude larger than 4 ...