GNGTS 2022 - Atti del 40° Convegno Nazionale

GNGTS 2022 Sessione 3.1 393 value is observed at about 34 km in the Calabrian arc and the Apennines thrust and fold belts with a sharp thermal gradient along the Tyrrhenian coastlines. Acknowledgments. This project is funded by Eni. References A. Tanaka, Y. Okubo and O. Matsubayashi: Curie point depth based on spectrum analysis of the magnetic anomaly data in East and Southeast Asia // pp. 461–470. B. Della Vedova, S. Bellani, G. Pellis and P. Squarci: Deep temperatures and surface heat flow distribution . In G.B. Vai and I.P. Martini (Eds.), Anatomy of an orogen: The Apennines and adjacent Mediterranean basins // pp. 65–76. B. Mather, and J. Fullea: Constraining the geotherm beneath the British Isles from Bayesian inversion of Curie depth: integrated modelling of magnetic , geothermal, and seismic data // pp. 839-850. C. Bouligand, J.M.G. Glen and R.J. Blakely: Mapping Curie temperature depth in the western United States with a fractal model for crustal magnetization. C. Lin, F. Berntsson, Z. Zhang, P. Wang, J. Wu and T. Xu: Seismically constrained thermo-rheological structure of the eastern Tibetan margin: implication for lithospheric delamination // pp. 122–134. I. Artemieva: Lithosphere: an interdisciplinary approach. Cambridge University Press // pp. 794. V. Cermak, and L. Bodri: Two-dimensional temperature modelling along five east European geotraverses // pp. 133– 163. Y. Kelemework, M. Fedi, and M. Milano: A review of spectral analysis of magnetic data for depth estimation // pp. J33-J58. Fig. 1 - Curie depth points map (a) estimated using spectral methods (Kelemework et al. , 2021) and 3D thermal distribution model (b) constrained by the Curie points, beneath Southern Italy.