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  • Geothermal and rheological regime in the Po plain sector of Adria (Northern Italy)
  • data are used to estimate upper crustal geotherms, which are subdivided into four groups taking into considerations the following factors: i) presence/absence of relevant fluid circulation; ii) conductive thermal refraction; iii) recent sedimentation
  • , and iv) other disturbing tectonothermal processes (e.g., recent tectonics). Using the estimated crustal structure and composition and the best-fitting geotherm, a representative strength envelope is obtained. - (NF)