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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)
  • 2012
  • Several geothermal fields are located in a NE-SW trend along a structural lineament around the Sivas basin. By evaluating the rocks of the Late Miocene-Early Pliocene Kızılırmak Formation, it was determined that fissure axes developed within Ortaköy
  • a result of NW-SE-directed compression, which was also responsible for the formation of the Sivas Backthrust. Ground-penetrating radar studies have shown that the thickness of fissure fills within the fissure-ridge-type travertines of the Ortaköy geothermal
  • 2012
  • This article discusses the character of post-mining potentials and their role in regional development in a German and Slovenian mining region. The many possible uses often include renewable energies (biomass, geothermal energy), or tourism (museums
  • 2012
  • Alterite ; Bauxite ; Chemical erosion ; Definition ; Earth surface processes ; France ; Geological map ; Geothermics ; Laterite ; Lithology ; Mining resources ; Natural hazards ; Natural resources ; Palaeogeography ; Periglacial features
  • 2012