GNGTS 2022 - Atti del 40° Convegno Nazionale

GNGTS 2022 Sessione 1.3 177 oxides. In addition, we compare the results obtained with the seismicity distribution (https:// www.usgs.gov/programs/earthquake-hazards/national-earthquake-information-center-neic ), as well as the depth of the Curie point (Li et al., 2019), and the effective elastic thickness obtained from isostatic analyses, in order to improve our understanding of the geodynamic setting of the area. References Agard, P., et al. , 2011. Zagros orogeny: A subduction-dominated process . Geological Magazine, 148(5–6), 692–725. https://doi.org/10.1017/S001675681100046X Conolly, 2005. Computation of phase equilibria by linear programming: A tool for geodynamic modeling and its application to subduction zone decarbonation . Earth and Planetary Science Letters, 236, 524-541. Khorrami et al. , 2019. An up-to-date crustal deformation map of Iran using integrated campaign-mode and permanent GPS velocities . Geophys. J. Int., 217, 832–843. Koulakov, 2011. High ‐ frequency P and S velocity anomalies in the upper mantle beneath Asia from inversion of worldwide traveltime data . Journal of Geophysical Research, 116, B04301, doi:10.1029/2010JB007938. Li et al., 2019. A global reference model of Curie-point depths based on EMAG2 . Scientific Reports, |7:45129 | DOI: 10.1038/srep45129. Mahmoodabadi, M., et al. , 2020. Shear wave velocity structure of the upper-mantle beneath the northern Zagros collision zone revealed by nonlinear teleseismic tomography and Bayesian Monte-Carlo joint inversion of surface wave dispersion and teleseismic P-wave coda . Physics of the Earth and Planetary Interiors, 300, 106444. https:// doi.org/10.1016/j.pepi.202 Manaman, N.S. and Shomali, H., 2010. Upper mantle S-velocity structure and Moho depth variations across Zagros belt, Arabian–Eurasian plate boundary . Physics of the Earth and Planetary Interiors, 180, 92–103 Mohammadi, N., et al. , 2013. New constraints on lithospheric thickness of the Iranian plateau using converted waves . Journal of Seismology 17:883–895 DOI 10.1007/s10950-013-9359-2. Motaghi, K., et al. , 2017. Underplating along the northern portion of the Zagros suture zone, Iran . Geophys. J. Int., 210, 375–389. Mouthereau, F., 2011. Timing of uplift in the Zagros belt/Iranian plateau and accommodation of late Cenozoic Arabia- Eurasia convergence. Geological Magazine, 148(5–6), 726–738. https://doi.org/10.1017/S0016756811000306 Priestley, K. and McKenzie, D. 2006. The thermal structure of the lithosphere from shear wave velocities . Earth and Planetary Science Letters, 244, 285–301. Wortel, M.J.R. and Spakman, W., 2000. Subduction and slab detachment in the Mediterranean-Carpathian region . Science, 290, 1910–17.